of Science antr &rt of tfje (Committee of 9 Oxygen and Nitrogen - - 12-47 Sulphur - 0-71 Ash - - - 2-20 Water - 9-52 100-00 15 See Percy's Metallurgy, Fuel, p. 327. A solid, compact, uon-caking coal. 87. " Mother of coal " from the surface of the heathen coal. 88. "Upper Four-foot coal." Dowlais, S. Wales. Analysed by E. RiJey, after desiccation. Carhon - 89-33 Hydrogen - 4-43 Oxygen - - ^3-25 Nitrogen - - 1-24 Sulphur - 0-55 Ash - - 1-20 100-00 See Percy's Metallurgy, Fuel, p. 328. A bright thin splintering non-caking coal used in blast furnaces. 89. " Rhes Las " or brassy coal. Dowlais, S. Wales. Analysed by E. Riley, after desiccation. Carbon - 88-13 Hydrogen - 4-51 Oxygen - - - - 2-94 Nitrogen - 1-41 Sulphur - 1-01 Ash - - 2-00 100-00 See Percy's Metallurgy, Fuel, p. 328. A small splintering non- caking coal used in forges. 90. " Bargoed Big coal." Dowlais, S. Wales. Analysed by E. Riley, after desiccation. Carbon - - 87-62 Hydrogen - 4-34 Oxygen - 2-52 Nitrogen - 1-13 Sulphur - - 1-07 Ash - .... 3-32 100-00 See Percy's Metallurgy, Fuel, p. 328. A small splintering non- caking coal used in blast furnaces. 91. " Tomo yard coal." Dowlais, S. Wales. Analysed by E. Riley, after desiccation. Carbon - - 82-60 Hydrogen - 4-28 Oxygen - 3-44 1C Nitrogen - - 1-28 Sulphur - 1-22 Ash - 7-18 100-00 See Percy's Metallurgy, Fuel, p. 328. A thin banded non-caking coal, not good for blast furnaces. 92. Cannel coal. Kirkless Hall and Hendley Colliery, near Wigan, Lancashire. 93. Very compact Cannel coal. Channock Chase, Stafford- shire. Communicated by Mr. McCleun. 94. Cannel coal. Dukinfield Colliery, Ashton-under-Lyne, Staffordshire. Analysed by C. Tookey. Carbon - 83-25 Hydrogen - 5-75 Oxygen and Nitrogen - 5-06 Sulphur - 0-86 Ash (grey) - - 3-48 Water - - - - - 1-60 100-00 See Percy's Metallurgy, Fuel, p. 330. It yields 63 '25 per cent, of coke and 35* 15 per cent, of volatile gaseous matter. 95. Smooth Cannel coal. Leeswood Green Colliery, Mold, Flintshire. Analysed by C. Tookey. Carbon - - -79-87 Hydrogen - - - - 5-78 Oxygen and Nitrogen - 8-09 Sulphur - 0-57 Waier- - - - 2-84 Ash - - 2-85 100-00 See Percy's Metallurgy, Fuel, p. 330. It yields 43-40 per cent, of volatile gaseous matter. 96. Curley Cannel coal. Leeswood Green Colliery, Mold, Flintshire. Analysed by C. Tookey. Carbon - - 77-81 Hydrogen - - 8-47 Oxygen and Nitrogen - - -6-32 Sulphur - 0-71 Water- - -068 Ash - - 6-01 100-00 17 See Percy's Metallurgy, Fuel, p. 328. It yields 92 '08 per cent, of volatile gaseous matter. 97. Cannel Coal. Leeswood Green Colliery, Mold, Flintshire. A more earthy looking bed lying helow No. 100 and yielding 30 '50 per cent, of ash. 98. Seaton Burn steam coal, or Ravensworth West Hartley, from Seaton Burn Colliery, Northumberland. Analysed by A. Dick, after desiccation. Carbon - 78-65 Hydrogen - - 4-65 Oxygen and Nitrogen - - - 13-66 Sulphur - - - 0-55 Ash 2-49 100-00 See Percy's Metallurgy, Fuel, p. 322. A non-caking coal. 99. Thick coal. Russell's Hall Colliery, Dudley, South Staffordshire. The finest quality set aside for making smiths' coke. It is one of the brilliant bituminous bands in the coal. 100. Main coal. Broughton Coal Company, Wrexham, Den- bighshire. Analysed by W. J. Ward. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - - Water - 100-0 See Percy's Metallurgy, Fuel, p. 333. A dull thin banded coal, yielding 61 38 per cent, of coke. 101. Crank coal. Broughton Colliery, Wrexham, Denbigh- shire. Analysed by W. J. Ward. Carbon - 81-29 Hydrogen - - 4-53 Oxygen and Nitrogen - - 6-77 Sulphur -r - 0-91 Ash - - -2-50 Water - 4-10 100-00 See Percy's Metallurgy, Fuel, p. 333. A very dull and earthy looking coal, yielding 68-80 per cent, of coke. U 61955. 18 102. Bituminous coal, No. 1. Risca Colliery, Newport, Monmouthshire. Analysed by W. J. Ward. Carbon - - - 80-08 Hydrogen - 5-03 Oxygen and Nitrogen - -5-29 Sulphur - 3-42 Ash (greyish white) - 5 05 Water - - - - 1-13 100-00 See Percy's Metallurgy, Fuel, p. 333. A banded coal, yielding 64 -72 per cent, of firm and coherent coke. 103. Bituminous coal, No. 2. Risca Colliery, Newport, Monmouthshire. Analysed by W. J. Ward. Carbon - - 75-49 Hydrogen - -4-73 Oxygen and Nitrogen - - -6-78 Sulphur - 1-21 Ash (greyish white) - - 10-67 Water - -1-12 100-00 See Percy's Metallurgy, Fuel, p. 333. A compact banded coal, yield- ing 68-88 per cent, of firm and coherent coke. 104. " Cae David " coal. Tywith Colliery, Llynvi Valley, Bridgend, Glamorganshire. Used at the Tonddu Ironworks.. Analysed by W. J. Ward. Carbon - - - 82-26 Hydrogen - 5-28 Oxygen and Nitrogen - - - 5-96 Sulphur - 1-25 Ash - - - 4-18 Water 1-07 100-00 See Percy's Metallurgy, Fuel, p. 334. A thin banded coal, yielding 66 38 per cent, of coke. 105. " Nine-foot " coal. Llynvi Coal and Iron Company, Bridgend, Glamorganshire. Analysed by W. J. Ward. Carbon - - - - 87-61 Hydrogen - - 4-73 Oxygen and Nitrogen - 3-55 Sulphur - 1-07 Ash - - 2-38 Water- ... - 0-66 100-00 19 See Percy's Metallurgy, Fuel, p. 334. A thin banded, small splinter- ing coal, yielding 79 -90 percent, of coke. 106. " Six-foot " coal. Llynvi Coal and Iron Company, Bridgend, Glamorganshire. Analysed by W. J. Ward. Carbon - 87-85 Hydrogen - - 4-67 Oxygen and Nitrogen - - - 3-77 Sulphur - - 1-07 Ash - - 2-00 Water- - 0-64 100-00 See Percy's Metallurgy, Fuel, p. 334. A brilliant small splintering coal, yielding 79-72 per cent, of coke. 107. " Duffryn " coal. Llynvi Coal and Iron Company, Bridgend, Glamorganshire. Analysed by W. J. Ward. Carbon - 84-75 Hydrogen - 4-65 Oxygen and Nitrogen - - 5-04 Sulphur - 0-76 Ash - - 3-93 Water- - 0-87 100-00 See Percy's Metallurgy, Fuel, p. 334. A small splintering coal, yield ing 76 92 per cent, of coke. 108. " Cae David " coal. Llynvi Coal and Iron Company, Bridgend, Glamorganshire. Analysed by W. J. Ward. Carbon 84-10 Hydrogen - 4-76 Oxygen and Nitrogen - -3-79 Sulphur - 1-28 Ash - - - 5-43 Water- - 0-64 100-00 See Percy's Metallurgy, Fuel, p. 334. A thick banded compact coal,, yielding 76-12 per cent, of coke. 109. " Yard " coal. Llynvi Coal and Iron Company, Bridgend, Glamorganshire. Analysed by W. J. Ward. Carbon - - 86-67 Hydrogen - 4-77 Oxygen and Nitrogen - - 4-30 Sulphur - 0-88 B 2 20 Ash - - 2-63 Water- - - - - 0-75 100-00 See Percy's Metallurgy, Fuel, p. 334. A banded small splintering coal, yielding 76*86 per cent, of coke. 110. " Victoria " coal. Llynvi Coal and Iron Company, Bridgend, Glamorganshire. Analysed by W. J. Ward. Carbon - - - 86-59 Hydrogen - 4-98 Oxygen and Nitrogen - -4-52 Sulphur - 0-93 Ash - - - 2-00 Water- - .0-98 100-00 See Percy's Metallurgy, Fuel, p. 334. A broad banded, small splin- tering coal, yielding 73- 16 per cent, of coke. 111. Top and bottom coal. No. 2 vein, Dunraven Colliery, Pontypridd, Glamorganshire. Analysed by W. J. Ward. The average of the two portions gives Carbon - 86-81 Hydrogen - - 4-51 Oxygen and Nitrogen - - -2-75 Sulphur - 1-75 Ash - - 3-40 Water - - - 0-78 100-00 See Percy's Metallurgy, Fuel, p. 334. A small splintering coal, yielding 86-81 per cent, of coke. 112. " Imperial Merthyr " coal. Aberdare, Glamorganshire. Analysed by W. J. Ward. Carbon - 88-34 Hydrogen - 4-06 Oxygen and Nitrogen - - 3-18 Sulphur - - 4-66 Ash - - 2-93 Water- - - 0-83 100-00 See Percy's Metallurgy, Fuel, p. 334. A bright, splintering coal, yielding 87 '54 per cent, of coke. Communicated by Livingston, Richards, and Almonds. 21 113. " Cory's Merthyr " coal. Aberdare, Glamorganshire. Analysed by W. J. Ward. Carbon - - - 86-80 Hydrogen - - 4-25 Oxygen and Nitrogen - 3*06 Sulphur - - - 0-83 Ash - - - 4-40 Water- - - - 0-66 100-00 See Percy's Metallurgy, Fuel, p. 334. A thin banded, splintering coal, yielding 84-42 per cent, of coke. 114. "Nine foot" coal. Bute pit, Hirvain, Aberdare, Glamorganshire. Analysed by W. J. Ward. Carbon - - 90-41 Hydrogen - - 3-97 Oxygen and Nitrogen - -2-20 Sulphur - 0-78 Ash - - - i-9o Water- - - 0-89 100-00 See Percy's Metallurgy, Fuel, p. 334. A semi-anthracitic, thin splintering, non-caking coal. Its particles slightly rounded on heating. Communicated by A. Tyler. 115. Top and bottom coal. No. 2 vein. Rhondda Waterfall Colliery, Glyn Neath, Glamorganshire. Analysed by W. J. Ward. The average of the two portions gives Carbon - 84-17 Hydrogen - 4-12 Oxygen and Nitrogen - - - 2 36 Sulphur - - 2-19 Ash - - 6-37 Water- - - - - 0-79 100-00 See Percy's Metallurgy, Fuel, p. 334. A bright thick banded coal, yielding 84-04 per cent, of coke. 116. " Nine foot " coal. Venallt Colliery, Glynabont, Neath, Glamorganshire. Analysed by W. J. Ward. Carbon Hydrogen Oxygen and Nitrogen Sulphur Ash - Water - 89-26 3-75 3-25 0-74 1-43 1-57 100-00 22 See Percy's Metallurgy, Fuel, p. 334. Yields 90 86 per cent, of coke. Communicated by W. Gregory, 1871. 117. Venalt coal, No. 1< Glynabont, Neatb, Glamorgan- shire. Analysed by W. J". Ward. Carbon - - - 88-85 Hydrogen - 4-22 Oxygen and Nitrogen - 3-15 Sulphur - 1-30 Ash - - 1-77 Water- - - 0-71 100-00 See Percy's Metallurgy, Fuel, p. 334. A dull coal, yielding 87 20 per cent, of coke. Communicated by W. Gregory, 1871. 118. Venallt coal, No. 2. Glynabont, Neatb, Glamorgan- shire. Analysed by W. J. Ward. Carbon - 85 00 Hydrogen - 3-93 Oxygen and Nitrogen - -2-24 Sulphur - 2-18 Ash - - 5-85 Water- - 0-80 100-00 See Percy's Metallurgy, Fuel, p. 334. A dull, banded coal, yielding 87 74 per cent, of coke. 119. " Wain-y-Coed " coal. Pontardawe, Swansea, Glamorgan- shire. Analysed by W. J. Ward. Carbon - - - 89-92 Hydrogen - - 4-32 Oxygen and Nitrogen - - 2-37 Sulphur - 0-78 Ash (red) - - 1-90 Water- - 0-71 100-00 See Percy's Metallurgy, Fuel, p. 335. A thin splintering coal, yield- ing 86-04 per cent, of coke. Communicated by the Primrose Coal Com- pany, 1870. 120. " Primrose " coal from the Primrose Colliery, Pontardavve, Swansea, Glamorganshire. Analysed by W. J. Ward. Carbon - - 88-83 Hydrogen - 4-25 Oxygen and Nitrogen - -2-41 Sulphur - 0-77 23 Ash (red) - - - 3-13 Water - - - 0-61 100-00 See Percy's Metallurgy, Fuel, p. 335. A thin splintering coal, yield- ing 83-82 per cent, of coke. Communicated by the Primrose Coal Company, 1870. 121. No. 3 coal. Nant-y-Moel Colliery, Ogmore Valley, Glamorganshire. Analysed by W. J. Ward. Used at the Tonddu Ironworks. Carbon - - 86-67 Hydrogen - - 5-03 Oxygen and Nitrogen - -4-44 Sulphur - 1-15 Ash - 1-63 Water- - 1-08 100-00 See Percy's Metallurgy, Fuel, p. 335. In small fragments. Yields 71-70 per cent, of coke. 122. Anthracite from Landshipping Colliery, Haverfordwest, Pembrokeshire. Analysed by W. J. Ward. As sent. Dried at 212 F. Carbon - - 91-05 92-35 Hydrogen - 2-80 2-85 Oxygen and Nitrogen - 1-72 1-74 Sulphur- - 0-98 0-99 Ash (light red) - - 2-05 2-07 Water - 1-40 100-00 100-00 See Percy's Metallurgy, Fuel, p. 335. A brilliant, compact, broad- banded, non-caking coal. 123. "Upper four foot seam/' Blaen Rhondda Colliery, Glamorganshire. Analysed by W. J. Ward. Carbon - - 86-49 Hydrogen - 3-69 Oxygen and Nitrogen - -3-08 Sulphur . 0-91 Ash - - 4.75 Water - -1-08 100-00 See Percy's Metallurgy, Fuel, p. 335. A dull, small splintering, non- caking coal. 24 124. Hafod coal. Glamorganshire. Analysed by W. J. Ward. Carbon - 86-95 Hydrogen - 4-84 Oxygen and Nitrogen - -4-64 Sulphur - - 0-64 Ash - - 2-05 Water - - - - 0-88 100-00 See Percy's Metallurgy, Fuel, p. 335. A bright, brittle coal, yielding 76 87 per cent, of coke. 125. Anthracite. Capel Ifan Colliery, Caermarthenshire. Analysed by W. J. Ward after desiccation. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - 100-00 See Percy's Metallurgy, Fuel, p. 569, where the analysis includes 1 -25 per cent, of water. A brilliant and compact coal. Total volatile matter 6 '05 per cent. Communicated by A. C. Miller. 126. Anthracite suitable for malting. From the Deep Stanllyd Big Vein, Llandebie, Caermarthenshire. A bright compact coal. 127. Anthracite from the " Pump Quart " Vein, Llandebie, Caermarthenshire. A bright and somewhat brittle, pyritous coal, containing " Mother of coal." 128. Anthracite from the "Pump Quart" Vein, Llandebie, Caermarthenshire. A very bright and compact coal, free from " Mother of coal." 129. Anthracite from Llangennech Colliery, Llanelly, Gla- morganshire. A steam coal. Analysed by W. J. Ward. Carbon - - - - 86-32 Hydrogen - - 3-09 Oxygen and Nitrogen - 4.29 Sulphur - - 0-66 Ash (pale red) - - 4-77 Water- - - 0-87 100-00 25 See Percy's Metallurgy, Fuel, p. 569. A dull fibrous coal, yielding 85-08 per cent, of firm lustrous coke. 130. "Grey Gog" seam. Trimsaran Colliery, Kidwelly, Caermarthen shire, without band. Analysed by W. J. Ward. Carbon - - 85-86 Hydrogen - 3-51 Oxygen and Nitrogen - -2-47 Sulphur - 0-80 Ash (white) - - 5-87 Water- - 1-49 100-00 See Percy's Metallurgy, Fuel, p. 570. A bright, small splintering anthracite, yielding 91-88 per cent, of coke. 131. The " Green " seam. Trimsaran Colliery, Kidwelly, Caermarthenshire. Analysed by W. J. Ward. Carbon - 90-53 Hydrogen - - - 3-61 Oxygen and Nitrogen - - -1-89 Sulphur - 1-07 Ash (red) - 1-30 Water- - 1-60 100-00 See Percy's Metallurgy, Fuel, p. 570. A bright, small splintering anthracite, yielding 90 90 per cent, of coke. 132. The " Drap Yein " top coal. Trimsaran Colliery, near Kidwelly, Caermarthenshire. An earthy coal, with transverse fibration due to pressure. 133. The " Drap Vein " bottom coal. Trimsaran Colliery, near Kidweily, Caermarthenshire. An irregular thin-banded coal. 134. " Smokeless steam coal " from Trimsaran Collieries, near Kidwelly, Caermarthenshire. Composed of equal parts by weight of two seams. Analysed in bulk by W. J. Ward after desiccation. Carbon - 90-51 Hydrogen - - 3-85 Oxygen and Nitrogen - -2-30 Sulphur - 0-80 Ash (red) - 2-54 100-00 Both are bright, small splintering coals. 26 135. Rhondda coal. Pwllfaron Colliery, Glyn Neath, Gla- morganshire. Analysed by W. J. Ward. Carbon - 88-25 Hydrogen - 3-71 Oxygen and Nitrogen - -2-09 Sulphur - 0-84 Ash (dark greyish red) - 4-13 Water - - 0-98 100-00 See Percy's Metallurgy, Fuel, p. 569. An anthracite in small dull pieces, yielding 92-f>9 per cent, of coke. 136. "Duffryn" coal. Dynevor, Duffryn Colliery, Neath, Glamorganshire. A dull irregularly banded coal. 137. " No. 2 Rhondda " coal. Top portion. Glyn Corrwg Colliery, Cardiff. Analysed by W. J. Ward. Carbon - b6-7l Hydrogen - 4-71 Oxygen and Nitrogen - -3-20 Sulphur - 1-53 Ash (pink) - 3-06 Water- - 0-79 100-00 See Percy's Metallurgy, Fuel, p. 569. A thin-banded, decaying cojil, yielding 80-72 per cent, of coke in concentric layers. 138. "No. 2 Rhondda" coal. Middle portion. Glyn Corrwo Colliery, Cardiff. Analysed by W. J. Ward. Carbon - 83-99 Hydrogen - 4 42 Oxygen and Nitrogen - 2-42 Sulphur - - 2-69 Ash (red) - 5-75 Water- 0-73 100-00 See Percy's Metallurgy, Fuel, p. 569. A dull coal, mostly decayed to powder, yielding 81-08 per cent, of coke in concentric layers. 139. "No. 2 Rhondda" coal. Bottom portion. Glyn Corrwg Colliery, Cardiff. Analysed by W. J. Ward. Carbon - - 84-99 Hydrogen - 4-39 Oxygen and Nitrogen - - 3-70 27 Sulphur - 1-49 Ash (pink) - 4-83 Water- - 0-60 100-00 See Percy's Metallurgy, Fuel, p. 569. A moderately bright, small splintering coal, yielding 80 52 per cent, of coke in concentric layers. 140. " Six feet " or top coal. Great Western Colliery, Ponty- pridd, Glamorganshire. A dull, thin splintering coal. 141. " Four feet " or middle coal. Great Western Colliery, Pontypridd, Glamorganshire. A moderately bright, brittle coal. 142. " Four feet " coal. Cymmer Colliery, Porth, Glamorgan- shire. A bright coal. 143. " Nine feet " coal. Cymmer Colliery, Porth, Glamorgan- shire. A rather dull coal. 144. " No. 2 Rhondda " coal. Corrwg Fechan Colliery, Glyn Corrwg, Cardiff. A rather dull, splintery coal. 145. Anthracite from the upper part of Penygraig vein, No. 2 Rhondda. Penygraig Colliery, Cwm Click, near Pontypridd, Glamorganshire. Analysed by W. J. Ward. Carbon - 85-79 Hydrogen - 3-71 Oxygen and Nitrogen - 2' 17 Sulphur - 1-89 Ash (reddish grey) - 5-25 Water - 1-19 100-00 See Percy's Metallurgy, Fuel, p. 570. Broken down to small fragments. 146. Anthracite from the lower part of Welsh vein, No. 3 Rhondda. Penygraig Colliery, Cwm Click, near Pontypridd, Glamorganshire. Analysed by W. J. Ward. 28 Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash (pale red) - Water - 100-00 See Percy's Metallurgy, Fuel, p. 570. Breaks into small, dull pieces. 147. Anthracite from the lower seam. Bonville Court Colliery, Saundersfoot, Pembrokeshire. A bright, compact coal, with conchoidal fracture. 148. Anthracite from the same locality as No. 147. A bright, banded coal showing iridescent colours. 149. " Kilgetty " coal. Kilgetty Colliery, Saundersfoot, Pem- brokeshire. A brilliant banded coal. 150. Anthracite from Moreton Colliery, Saundersfoot, near Tenby, Pembrokeshire. A bright banded coal. 151. The " six foot " seam. Mynydd-Bach-y-glo Colliery. Swansea, Glamorganshire. A dull and fibrous coal, used for household purposes, gas-making, and smelting. Communicated by W. P. Struve. 152. The " three foot " seam. Mynydd-Bach-y-glo Colliery, Swansea, Glamorganshire. An irregular dull coal, very free from sulphur and excellent for foundry and smelting purposes. Communicated by W. P. Struve. 153. The "two foot" vein. Mynydd-Bach-y-glo Colliery, Swansea, Glamorganshire. A dull, rather compact coal, suitable for household purposes, gas- making, and smelting. Communicated by W. P. Struve. 154. " Ynysgreinion " anthracite, smokeless steam coal, used also for malting. Victoria Coal and Iron Company, Swansea, Yale Ystalyfera, Glamorganshire. Analysed by W. J. Ward. Carbon - 89-53 Hydrogen - 3-66 Oxygen and Nitrogen - -1-98 Sulphur - 1-38 Ash (red) - 1-75 Water- - - - 1-70 100-00 29 See Percy's Metallurgy, Fuel, p. 570. A very brilliant, small splinter- ing coal, yielding 91-10 pev cent. coke. 155. " Ynysgeinion" malting coal No. 2. Ystalyfera, Gla- morganshire. Analysed by W. J. Ward. Carbon - - - - 90-49 Hydrogen - - - 3-97 Oxygen and Nitrogen - - 0-88 Sulphur - 1-18 Ash (pale red) - 2-20 Water- - - - - 1-28 100-00 A brilliant, small splintering coal. 156. " Ynyscedwin " coal No. 1. Near Swansea, Glamorgan- shire. Analysed by W. J. Ward. Carbon - - - 90-48 Hydrogen - - 3-77 Oxygen and Nitrogen - -1-95 Sulphur - - - 0-54 Ash (pale reddish grey) - 1/95 Water- - 1-31 100-00 A compact, not very brilliant coal. 157. " Ynyscedwin " coal No. 2. Near Swansea, Glamorgan- shire. Analysed by W. J. Ward. Carbon - 87-61 Hydrogen - ..-.. 3-62 Oxygen and Nitrogen - -3-10 Sulphur - 3-81 Ash (white) - - - 3-55 Water - 1-31 100-00 Brilliant, thin banded, and compact. 158. " Ynyscedwin " coal No. 3. Near Swansea, Glamorgan- shire. Analysed by W. J. Ward. Carbon - 87-76 Hydrogen - 3-76 Oxygen and Nitrogen - -2-75 Sulphur . 0-78 Ash (pale, reddish grey) - 3-70 Water- - - 1-25 100-00 Brilliant, banded, and compact. 30 159. ' : Ynyscedwin " coal No. 4. Near Swansea, Glamorgan- shire. Analysed by W. J. Ward. Carbon 86 67 Hydrogen - 3*24 Oxygen and Nitrogen - 3-15 Sulphur 0'74 Ash (pale, reddish grey) - 5-00 Water - -1-20 100-00 A compact and dull coal. 160. "Four feet" seam. Maedy Colliery, Pontypridd, Gla- morganshire. A steam coal. Not very bright, but banded. Communicated by E. S. Judkins. 161. Coals No. 1 and 2 from Glamorgan Colliery, Pontypridd, Glamorganshire. Both are bright and banded. 162. Coals No. 3 and 4 from Glamorgan Colliery, Pontypridd, Glam organshir e. Bright and thin splintering. 163. Coals No. 5 and 6 from Glamorgan Collier}', Pontypridd, Glamorganshire. One is dull, the other brighter. 164. " Black vein " steam coal. Celynen Colliery, Abercarn, Monmouthshire. A bright, thin banded coal. 165. Tyrcenol coal, Used in copper smelting at Hafod Works, near Swansea. Mixed with equal parts of Mynydd Newydd and Pentrefelin coals. Analysed by A. Dick after desiccation. Carbon - - 76 -SI Hydrogen - 3-42 Oxygen and Nitrogen - -5-65 Sulphur - 1-96 Ash - - 12-16 100-00 See Percy's Metallurgy, Fuel, p. 350, where analyses of the ashes of these coals are also given. In fragments. 166. " Top Coal." Henlis Coal and Firebrick Works, New- port, Monmouthshire. Analysed by W. J. Ward. 31 Carbon - - 75-85 Hydrogen - 4-74 Oxygen and Nitrogen - 7*72 Sulphur - - -1-09 Ash (grey) - - - 8-87 Water - - - -1-73 100 -CO See Percy's Metallurgy, Fuel, p. 570. Yields 69-40 per cent, of coke. Communicated by J. C. Hill, 1874. 167. " Bottom coal." Henlis Coal and Firebrick Works, Newport, Monmouthshire. Analysed by W. J. Ward. Carbon - - 74-90 Hydrogen - 4-98 Oxygen and Nitrogen - - -8-16 Sulphur - 1-69 Ash (reddish grey) - - 8-17 Water - - - - -2-10 100-00 See Percy's Metallurgy, Fuel, p. 570. Yields 65-60 per cent, of coke. Communicated by J. C- Hill, 1874. 168. "Smith coal," or 20-inch coal, Forest of Dean. Nearly the highest seam in the district. Bright and compact. 169. " Little Delf," Forest of Dean ; average thickness 20 in. Follows the Smith coal. Less compact and duller. 170. "Parkend High Delf," or "Lowry" coal, Forest of Dean ; average thickness 3 ft. 7 in. Follows the Little Delf. The only sort used at Parkend furnaces. Brilliant and compact. 171. Black shale. Parkend, High Delf Colliery, Forest of Dean. Analysed by C. Tookey. In small fragments. 172. " Starkey Delf," Forest of Dean ; average thickness 2ft. Follows the Parkend. Duller, compact, and thin banded. 173. " Rocky Delf," Forest of Dean ; average thickness 1 ft. Sin. Follows the Starkey. Compact, banded, alternately bright and dull. 174. "Churchway High Delf/ 5 or " Oaken Hill and Smart Delf," Forest of Dean; average thickness 1 ft. 11 in. 32 Follows the Rocky, and is followed by Churchway Low Delf. Rather dull, compact. 175. Bailey or Yorkley Delf, Forest of Dean ; average thickness 1 ft. 9 in. Follows the Churchway Delf, and is followed by Nags Head Delf. Thin banded, efflorescing and decayed. 176. " Whittington," Forest of Dean; average t ickness 2 ft. 6 in. Follows the Nags Head Delf. An earthy coal, very brown and res- inous looking. 177. " Coleford High Delf," Forest of Dean ; average thick- ness 5 ft. Follows the Whittington. Not very bright nor compact. 178. " Trenchard Coal," Forest of Dean ; averages 2 ft. Follows the Coleford High Delf, and is the lowest coal but one in the field. Dull, earthy, effloresced, and decayed. 179. " Top coal," Bagworth, Leicester. Dull and earthy, like cannel. Communicated by the OHyndon Iron Company, 1871. 180. " Middle coal," Bagworth, Leicester. \ r ery dull, thin banded, and compact. Communicated by the Glyndon Iron Company, 1871. 181. "Main coal/' Whitwick Colliery, Leicester. Analysed by J. W. Ward, 1875. Carbon - - 69-00 Hydrogen - 4-35 Oxygen and Nitrogen - - 10-78 Sulphur - 0-78 Ash (pinkish) - - 5-4:3 Water - - - - 9-67 100-00 See Percy's Metallurgy, Fuel, p. 570. Yields 58-14 per cent, of coke and 32 19 per cent, of volatile matter. 182. Coal from the Leeswood Green Colliery, Mold, Flint- shire, showing (i mother of coal." Very bright and compact, the mother of coal being the disintegrated parting between the solid layers. 183. " Arley Mine coal," Wigan, Lancashire ; considered the best coal in the district for house, gas, and coking purposes. Compact, iridescent, and slightly effloresced. 33 184. " Arley Mine coal," Wigan, Lancashire ; of a different structure from No. 187, and from a different part of the workings. Duller and more thinly banded. 185. Wigan cannel coal, in association with ordinary coal, which takes its place as the cannel dies away, so that the average total thickness is maintained. Communicated by C. Wright. 186. The ordinary Wigan coal, that accompanies the cannel oal, without any of the latter. A dull, very compact coal. Communicated by C. Wright. 187. "Thick" coal, or 6 ft. seam, Burnley Coalfield, from Bancroft Colliery, Padiham, Lancashire. A broad-banded, moderately bright coal. Communicated by Sir J. K. Shuttleworth. 188. " Roof coal/' Gawthorpe Colliery, in the Burnley Coal field, Lancashire. Bather dull and more thinly banded. Communicated by Sir J. K. Shuttleworth. 189. " Low Moor " coal ; hard ; Yorkshire. Very dull, compact, and thin banded. 190. " Low Moor " coal ; soft ; Yorkshire. Bright, with thin bands alternately bright and dull. 191. Iron pyrites in soft Low Moor coal. 192. " Hesley Silkstone " coal, near Barnsley, Yorkshire. Compact, thin banded, rather dull. Communicated by Newton, Chambers, and Co. 193. " Silkstone Gas " coal, near Barnsley, Yorkshire. Brighter and more thickly banded. Communicated by Newton, Chambers, and Co. 194. Steam coal, from near Barnsley, Yorkshire. Bright and moderately thin banded. Communicated by Newton, Chambers, and Co. 195. " Yorkshire coal," sample A. Analysed by W. J. Ward Carbon - 72-31 Hydrogen . 5-52 Oxygen and Nitrogen - -9-62 Sulphur - - 2-44: Ash (reddish grey) - 4-80 Water- - 5-31 100-00 U 61955. n 34 A very bright and compact coal, with a uniform, almost couchoidal fracture, and yielding 56*32 per cent, of coke. Communicated by Row. Winn. 196. "Yorkshire coal," sample B. Analysed by W. J. Ward. Carbon 74-05 Hydrogen - 5-25 Oxygen and Nitrogen - - JO- 38 Sulphur - 1-66 Ash (reddish grey) - - -2-64 Water - 6-02 100-00 Similar to the last, but the fracture is a little rougher. Yields 56-92 per cent, of coke. Communicated by Bow. Winn. 197. Coal from Fair Oak Colliery. Rather dull and irregularly banded. 198. " Fernhill " coal. Very bright and broad banded, with dull partings. 199. Sample from a mass of coal which ignited spontaneously in the Woolwich Gasworks in 1873. It was received as " New Pelton Gas Coal," and in a wet condition 150 tons of it were stored in a shed having only the front open ; and 2,000 tons of other coal were placed on the top, and no system of internal ventilation was adopted. It ignited after six months' storage, from May to November. This is not, properly speaking, a coal at all r but a mass of pyrites in which is imbedded a large quantity of the charcoal- like mother of coal. Communicated by C. Iceby. 200. " Six-foot " coal from Pentrefelin Colliery, near Swansea, Glamorganshire. Used in the Copper Smelting Works at Hafod. Mixed with equal parts of Mynydd Newydd and Tyrcenol coal. Analysed by A. Dick after desiccation. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - - - , 100-00 See Percy's Metallurgy, Fuel, p. 350. Moderately light and broad banded. 201. " Six-foot coal " from Mynydd Newydd Colliery, near Swansea, Glamorganshire. Used in copper smelting works at Hafod. Mixed with equal parts of Pentrefelin and Tyrcenol. Analysed by A. Dick after desic- cation. 85 Carbon Hydrogen Oxygen and Nitrogen Sulphur Ash - 100-00 See Percy's Metallurgy, Fuel, p. 350. Kather dull and small splintering. 202. Coal of the age of the Lower Oolites from the Brora Coalfield, Sutherlandsnire. (See Hull's Coalfields of Great Britain.) A perfectly black and compact coal, brighter than cannel coal. Com- municated by the Duke of Sutherland. FOREIGN COALS. EUROPEAN COALS. 203. Coal from Steyerdorf, Switzerland. Of Carboniferous age. Formerly supposed to belong to the Lias, having been misplaced by the inversion of the strata. Small fractured, solid, feebly banded. 204. Coal from the level at Courtres (Novelle?), Switzerland. Of Carboniferous age. Analysed by W. J. Ward. Carbon - 59-16 Hydrogen - 3-78 Oxygen and Nitrogen - 4-97 Sulphur - 3-48 Ash (pale red) - - 28-13 Water - - - - -48 100-00 See Percy's Metallurgy, Fuel, p. 336. Compact, dull, without band- ing and with irregular fracture. Yields a light coke. Communicated by McDougal Smith, 1865. 205. Coal from the upper or east gallery, Novelle, Switzerland.. Of Carboniferous age. A dark earthy lignite-like coal with irregular fracture. Yields 45 40 per cent, of a scarcely coherent coke and 10 95 per cent, of ash. Burns with a smoky yellow flame. Communicated by McDougal Smith, 1865. 206. Coal from Novelle, Switzerland. Of Carboniferous age. Yields 55 28 per cent, of coke and 2- 70 of ash. Burns with a smoky name and yields much gas, and decrepitates. Brilliant, compact, and resinous, with conchoidal fracture. Communicated by McDougal Smith, 1865. c 2 36 207. Coal from Servia, A very dark irregular lignite. 208. Cannel coal from Styria. A hard eaithy black shale. Used in the manufacture of gas at Vienna by the Imperial and Continental Gas Company. Communicated by E. W. Voelcher, 1876. AMERICAN COALS. 209. Coal from Springfield, Bay of Fundy, "Nova Scotia. Of Carboniferous age. Analysed by W. J. Ward. Carbon - 75-51 Hydrogen - 5-00 Oxygen and Nitrogen - - -9-37 Sulphur - 1-09 Ash (greyish white) - 5-05 Water - - - - 3-98 100-00 See Percy's Metallurgy, Fuel, p. 337. A dull, resinous looking coal with irregular fracture. Yields 64 94 per cent, of coke. Communicated by J. Livesey. 210. Glasgow and Cape Breton coal, Nova Scotia ; of Car- boniferous age. Analysed by W. J. Ward. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash (dark greyish red) Water - 300-00 Dull and compact in one part, decayed in another ; yields 62-74 per cent, of coke and 36-20 of volatile matter. Communicated by the Glasgow and Cape Breton Coal Company. 211. Coal from Schooner Pond, Nova Scotia ; of Carboniferous age. Analysed by W. J. Ward. Carbon ... Hydrogen Oxygen and Nitrogen - Sulphur ... Ash (dark greyish red) Water - - 100-00 It has an irregular fracture, and is effloresced and disintegrated. It yields 61 -90 per cent, of coke and 35-43 per cent, of volatile matter. Communicated by the Glasgow and Cape Breton Coal Company. 37 212. Cannel coal from Schooner Pond, Nova Scotia ; of Car- boniferous age. Analysed by W. J. Ward. Carbon - - - 63-72 Hydrogen - - 4-79 Oxygen and Nitrogen - Sulphur - Ash (red) Water - 100-00 See Percy's Metallurgy, Fuel, p. 337. A dull, massive coal, like cannel, yielding 63 1 1 per cent, of a hard and compact coke, and 35 64 per cent, of volatile matter. Communicated by the Schooner Pond Coal Company. 213. Coal from the Inter-colonial Company's Colliery, Pictou County, Nova Scotia. Of Carboniferous age. The seam called the "Lower Bunch," which is about 19 feet thick. A rather dull, compact, thin-banded coal. 214. Coal from the Inter-colonial Company's Colliery, Pictou County, Nova Scotia. Of Carboniferous age. The seam called " Upper Bunch," which is about 19 feet thick. A compact and thin-banded coal. 215. Coal from the Albion Mines, Pictou County, Nova Scotia. From the " Cage pit." Of Carboniferous age. The "Deep seam," 12 feet thick, yielding a good coal in three bands. It is dull and compact, with narrow bright bands. 216. Coal from the Albion Mines, Pictou County, Nova Scotia. Of Carboniferous age. The " Main seam," 38 feet thick, with some partings, also called the " Upper Bunch." A dull, thin-banded coal, with much " mother of coal." 217. Coal from " Mitchells adit," Pictou County, Nova Scotia. Of Carboniferous age. About 13 feet thick with some coarse coal. Bright, irregularly banded. 218. Coal from the Yale Colliery, Pictou County, Nova Scotia. Of Carboniferous age. The " Eight-foot " seam. Dull, thin-banded. 219. Coal from Vale Colliery, Pictou County, Nova Scotia. The outcrop of the 3-foot seam. Communicated by Gr. M. Dawson. 220. The Coal, Brick, and Pottery Company's seam, Pictou County, Nova Scotia. Of Carboniferous age. A coal 2 feet thick, worked with several feet of fire-clay. Irregularly banded, alternately dull and bright. 38 221. Coal from " Chimney corner," Cape Breton Island. Of Carboniferous age. Broad banded, with no bright layers and some very dusty. 222. Coal from Port Hood, Cape Breton Island. The main or " six foot " seam. Of Carboniferous age. Compact and thin-banded, but now completely effloresced and frag- mentary. 223. Coal from the Vancouvers Coal Mines and Land Company's Colliery, Vancouvers Island, British Columbia. Of Cretaceous age. Analysed by W. J. Ward. Carbon - - 72-29 Hydrogen - 5-58 Oxygen and Nitrogen - -6-36 Sulphur - 2-62 Ash - - 11-62 Water- - - - - 1-53 100-00 See Percy's Metallurgy, Fuel, p. 338. A black, dull, not clearly banded coal, in small pieces, yielding 57- 15 per cent, of coke. 224. Coal from Vancouvers Coal Mines and Land Company's Colliery, Vancouvers Island, British Columbia. Of Cretaceous age. Analysed by W. J. Ward. Carbon - 69-93 Hydrogen - 4-95 Oxygen and Nitrogen - - - 1 1 48 Sulphur - 0-74 Ash - - 9-70 Water- - 3-20 100-00 See Percy's Metallurgy, Fuel, p. 338. A rather dull, broad-banded, black coal, yielding 60-08 per cent, of coke. Communicated by Mr. Eobins, 1873. 225. Coal from Vancouvers Coal Mines and Land Company's Colliery, Vancouvers Island, British Columbia, Of Cretaceous age. Analysed by W. J. Ward. Carbon - 70-99 Hydrogen - - 5 19 Oxygen and Nitrogen - 10-20 Sulphur - 0-97 Ash - - 9-75 Water- - 2-90 100-00 39 See Peicy's Metallurgy, Fuel, p. 338. A rather dull, irregularly breaking, not clearly banded coal, yielding 62-15 per cent, of coke. Communicated by Mr. Robins, 1873. 226. Coal from near Nanaimo, Vancouvers Island, British Columbia. Of Cretaceous age. Analysed by W. J. Ward. Carbon - 73-28 Hydrogen - 5-37 Oxygen and Nitrogen - -11-44 Sulphur - 0-51 Ash (dirty buff) - - 6-63 Water 2-77 100-00 See Percy's Metallurgy, Fuel, p. 338. A black, moderately bright and compact, rather broad-banded coal, yielding 58 80 per cent, of coke and 38 43 per cent, of volatile matter. Communicated by the Admiralty. 227. Coal brought to England by H.M.S. " Discovery," discovered during the Arctic expedition in 1876. It occurs in 81 43' N. L. and 64 4' W. L. It is of Miocene age. A sample analysed by R J. Moss yielded- Carbon - - 75-49 Hydrogen - - 5-60 Oxygen and Nitrogen - - -9-89 Sulphur - - 0-52 Ash - - 6-49 Water- . . . 2-01 100-00 A black, lustrous, tender coal, in thin bands and with many trans- verse cracks. Yields 61 per cent, of coke. See Proc. Royal Dublin Society, N.S., vol. 1, p. 61. 228. " Black Diamond " or " Tower Vein " from Mount Diablo. About 40 miles South of San Francisco, California. A compact cannel-like coal, slightly banded. Communicated by J. Jouberton. 229. Colorado coal ; locality not stated. Dull, almost resinous, thin-banded. Communicated by W. Cope. 230. Coal from Canon City on the Arkansas river in Colorado, North America. Probably of Cretaceous age. A compact bright coal, indistinctly but thinly banded. Communi- cated by A. G. Renshaw, 1874. 231. Coal from the United States of Colombia, South America. Analysed by W. J. Ward. Carbon - - 76*45 Hydrogen - 4-88 Oxygen and Nitrogen - - 1 2 06 Sulphur - 0-25 Ash - - 1-25 Water- - - - - 5-11 100-00 See Percy's Metallurgy, Fuel, p. 339. A dull, very tender, thin- banded, non- caking coal. Communicated by the Admiralty, 1872. 232. Coal from the United States of Colombia. Analysed by W. J. Ward. Carbon - - - - 56-66 Hydrogen - - 4-08 Oxygen and Nitrogen - - 17-25 Sulphur - - 0-30 Ash - - - - - 2-63 Water- - 19-08 100-00 See Percy's Metallurgy, Fuel, p. 339. A very dull and tender black coal, in separate layers of compacted dust. Communicated by the Admiralty, 1872. 233. Coal from San Jeronymo, New Granada. Analysed by C. Tookey. Carbon - -' - 59-05 Hydrogen - 4-03 Oxygen and Nitrogen - - 10-54 Sulphur - - 0-54 Ash (nearly white) - - 16-68 Water- - 9-16 100-00 See Percy's Metallurgy, Fuel, p. 340. A tolerably compact and thin banded coal. 234. Coal from Brazil. Analysed by W. J. Ward. Carbon - 56-28 Hydrogen 3-87 Oxygen and Nitrogen - - -10*74 Sulphur - 0-56 Ash (white) - - 16-85 Water- - - - 11-70 100-00 See Percy's Metallurgy, Fuel, p. 340. A very dull and compact coal, yielding 59-60 per cent, of coke. It has occasional bright bands and splits along the bedding. Its composition is the same as some South Staffordshire coals. 41 235. Coal from the Province of S. Catherine's, Brazil. A dull, brownish black, compact coal, with irregular bright bands. 236. Coal from the Imperial Brazilian Collieries Company's mines, South Brazil. A dull, compact, banded coal, with occasional bright bands. 237. Coal from Punta Arenas or Sandy Point, Straits of Magellan. Analysed by W. J. Ward. Carbon - - - - 74-82 Hydrogen - 4-91 Oxygen and Nitrogen - - 8-93 Sulphur - 0-82 Ash - - 6-98 Water - - - - -3-54 100-00 See Percy's Metallurgy, Fuel, p. 341. A compact, dull, very feebly broad-banded coal, yielding 62 '80 per cent, of compact coke. Com- municated by the Admiralty, 1873. 238. Coal from Chili, near Coronel, 250 miles south of Valparaiso. Analysed by W. J. Ward. Carbon - - Hydrogen Oxygen and Nitrogen - Sulphur - - Ash ----- Water - 100-00 See Percy's Metallurgy, Fuel, p. 341. A bright, compact, feebly banded coal, yielding 60-56 per cent, of compact coke. 239. Coal from the South of Chili. Used for smelting copper, for which purpose it is mixed with two- thirds of its weight of Welsh coal. A dull coal, once compact, now effloresced and decayed. Communicated by the Copiapo Smelting Company, Caldera. 240. Anthracite from Peru. Brought by H. Bauerman from a 6 ft. bed at Poaten, in the Pampas of the Sierra, 40 miles north-east of Truxillo. Believed to be of Mesozoic age. Analysed by W. J. Ward. Carbon - - 82-70 Hydrogen _ 1-41 Oxygen and Nitrogen - - -0-85 42 Sulphur Ash - Water - 100-00 See Percy's Metallurgy, Fuel, p. 567. Brilliant, compact, with irregular fracture. A sample accompanies the raw coal which has been heated for a long time ; by this treatment the per-centage of sulphur was only reduced to 7-35 per cent., showing that this amount must exist in an organic combination. ASIATIC COALS. 241. Labuan coal from the north-west of Borneo. Contains small lumps of resin. Analysed by C. Tookey. Carbon - - 71-66 Hydrogen - 5 53 Oxygen and Nitrogen - -14-66 Sulphur - 0'40 Ash - - 1'95 Water- 5*80 100*00 See Percy's Metallurgy, Fuel, p. 342. A bright, compact coal, with irregular fracture and obscure bands, yielding 50-70 per cent, of semi- coherent coke. Communicated by Vice- Admiral Hope, 1872. 242. Labuan coal. Labuan Coal Company, Borneo. Ana- lysed by C. Tookey. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - Water - 100-00 See Percy's Metallurgy, Fuel, p. 342. A very compact, bright coal, with conchoidal fracture, resembling c:mnel coal, and having no band- ing. Yields 56 '10 of coke. Communicated by Vice-admiral Hope, 1872. 243. Labuan coal. Analysed by W. J. Ward, 1865. Carbon - 70-96 Hydrogen - 5 ' 57 Oxygen and Nitrogen - - 14-34 Sulphur 1-43 Ash (pale red) - 2*15 100-00 43 See Percy's Metallurgy, Fuel, p. 342. A dull, compact, thinly and obscurely banded coal, yielding 52-16 per cent, of coke. 244. Coal from Labuan, N.W. of Borneo. Sample from the surface outcrop obtained in 1851. Dull, resinous, banded. Communicated by J. Drummond, 245. Labuan coal. Analysed by W. J. Ward, 1865. Carbon - 71*56 Hydrogen - - 5*09 Oxygen and Nitrogen - - 14-47 Sulphur - 0-98 Ash (brownish red) - 2*45 Water - 5*45 100-00 See Percy's Metallurgy, Fuel, p. 342. Yields 51-02 per cent, of coke. It is a broad- banded, dull, effloresced coal, which contained, when received, pyrites, ferrous sulphate, and basic ferric sulphate. 246. Coal from Sumatra, called " Ranti " coal. Analysed by W. J. Ward, 1872. Carbon - 75*27 Hydrogen - 5*63 Oxygen and Nitrogen - -12-56 Sulphur - 0*49 Ash - 0*83 Water _ 5-22 100 '00 See Percy's Metallurgy, Fuel, p. 343. A very compact, moderately bright coal, in very broad ill-defined bands. Yields 54-58 per cent, of coke. 247. Coal from Sumatra, called " Soengei Doerian " coal Analysed by W. J. Ward, 1872. Carbon . 73-04 Hydrogen . 4.99 Oxygen and Nitrogen - _ 12-41 Sulphur - 1-08 Ash - - 1-43 Water - 7 '05 100-00 See Percy's Metallurgy, Fuel, p. 343. A very compact, moderately bright coal, with a very obscure but excessively fine banding. Yields 55-48 per cent, of coherent coke. 248. Coal No. l,from Tjitjalenka, Java. Analysed by W. J. Ward. 44 Carbon - - - 47 "91 Hydrogen - - 4*71 Oxygen and Nitrogen - - - 11*31 Sulphur - 0'74 Ash (buff) - - 23-32 Water - - - 12 '01 100 '00 A very dull, deep brown, very compact lignite, yielding 49 52 per cent, of non-coherent carbonaceous residue and 38 * 17 per cent, of volatile matter. Communicated by Bateman and Company, 1872. 249. Coal No. 2, from Tjitjalenka, Java. Analysed by W. J. Ward. Carbon - - - - 53-85 Hydrogen - - 3*59 Oxygen and Nitrogen - -11-17 Sulphur - .0*91 Ash (pale red) - - 8-15 Water - - - - 22-33 100 '00 A brown, earthy lignite, with occasional bright bands, yielding 46 '58 per cent, of a non-coherent carbonaceous residue and 31*09 per cent, of volatile matter. Communicated by Bateman and Company, 1872. 250. Coal from the Island of Formosa. A moderately bright, irregularly banded anthracite -like coal. Com- municated by the Admiralty, 1872. 251. Coal from the Bolan Pass, Beloochistan, West of India. An earthy, dark brown lignite. Communicated by.W. H. Sykes. 252. Coal from the Ranigimgi Coalfield, Bengal Colliery, of Ranigungi Coal Association. Dull, banded, compact, with a few thin bright bands ; with cylinders of coke produced from its dust. Communicated by A. J. Mackay. 253. Coal from the Ranigungi Coalfield, Damuda Valley, Bengal. Belongs to the Gondwana series of Carboniferous age, though with the type of flora which is Mesozoic in Europe. A compact, dull coal, with bright bands. 254. Coal from " Sanatoria " Coalfield, Bengal. Probably also of Gondwana series of Carboniferous age. A bright, compact, fine-banded coal. 255. Coal from Hyderabad, Deccan, India (No. 1). Analysed by W. J. Ward. 45 Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - Water - 100-00 See Percy's Metallurgy, Fuel, p. 345. A tender, irregularly banded, dull coal, yielding 54-74 per cent, of non-coherent coke. Communicated by J. G. Palmer, 1872, 256. Coal from Hyderabad, Deccan, India (No. 2). Analysed by W. J. Ward. Carbon - Hydrogen - Oxygen and Nitrogen - Sulphur - - Ash Water - ... 100-00 See Percy's Metallurgy, Fuel, p. 345. A very dull, banded, lignite- like coal, yielding 57 24 per cent, of non-coherent coke. Communicated by J. G. Palmer, 1872. 257. Coal from Takasima, in the island of Niphon, Japan. Analysed by W. J. Ward. Carbon - 79-26 Hydrogen - 5 86 Oxygen and Nitrogen - -8-76 Sulphur - - 0-11 Ash (pale red) - - 4*51 Water - - - - - 1-50 100-00 See Percy's Metallurgy, Fuel, p. 345. A friable, small splintering, not very brilliant coal, yielding 58 per cent, of tender coke. 258. Anthracite from China, locality unknown. Brought from Pekin. Analysed by C. Tookey. Carbon - 72-27 Hydrogen - - - 2-00 Oxygen and Nitrogen - -3-42 Sulphur - 0-41 Ash (sandy grey) - 19-00 Water - - - 2 90 100-00 See Percy's Metallurgy, Fuel, p. 348. A bright, compact, thin- banded coal, which does not cake in the slightest degree and gives 46 no illuminating gas on ignition. It yields 89*55 per cent, of car- bonaceous residue and 7 '55 per cent, of volatile matter. Communicated by the Admiralty. Obtained by James Hope. 259. Coal from the hills about 180 miles west of Pekin near Tung-chow; believed to be of Mesozoic age. (See Newberry, Am. Journ. Sci. XLII.) Analysed by C. Tookey. Carbon - - 85-3 Hydrogen - 4-50 Oxygen and Nitrogen - 3 39 Sulphur - 0-40 Ash (brownish red) - -5-82 Water- - 0-53 100-00 See Percy's Metallurgy, Fuel, p. 348. A very bright, large-fractured coal, yielding 83-47 per cent, of coke and 16-60 per cent, of volatile matter. In trial on board the ' ; Weasel " it was found to be equal or superior to the best Welsh steam coal. Communicated by the Admiralty. Obtained by James Hope. 260. Coal from the hills near Tseug-ko-ken, in the province of Pechili, and brought from Jehol in Tartary. Analysed by C. Tookey. Carbon - - 70-09 Hydrogen - 4-90 Oxygen and Nitrogen - 8-57 Sulphur - 0-77 Ash (grey) - 13-82 Water - - - 1-85 100-00 See Percy's Metallurgy, Fuel, p. 348. A bright, compact, thick- banded coal, yielding 63-15 per cent, of a firm coherent coke, and 35 per cent, of volatile matter containing much illuminating gas. Communicated by the Admiralty. 261. Coal from the hills near Tseng-ko-ken ; being part of the same parcel as No. 260, and having the same properties. Analysed by C. Tookey. Carbon 61-90 Hydrogen - 4-58 Oxygen and Nitrogen - -8-57 Sulphur - 0-68 Ash (grey) - - 22-62 Water - - 1-65 100-00 See Percy's Metallurgy, Fuel, p. 348. A duller, and more compact coal, yielding 31-30 per cent, of volatile matter. Communicated by the Admiralty. 47 262. Coal from China ; locality unknown. Brought by J. White. 1877. A very dull, earthy, lignite-like coal. 263. Coal from Hu-Is'iin (No. 1), China. Brilliant, compact, and thin banded. 264. Coal from Chang-chia Hill behind Po-fcu village, China, Rather tender, thin banded, alternately bright and dull. 265. Coal from Su feng bridge, China. B road banded, compact. 266. Coal from Shan-ti village, China, Bright, compact, thin banded. 267. Coal from Hu Is'un (No. 2), China. Bright, rather tender, irregularly banded. 268. Coal from Hsiwang-kan village, China. Bather dull, thin banded. 269. Coal from Lao Tsa Gulley, China. Dull, tender, obscurely banded. 270. Two varieties of Pung Chung coal, China. Both are rather dull and irregular. AUSTRALASIAN COALS. 271. Small samples of Australian coal, originally sent over to Sir B,. I. Murchison. These are severally : 1. Lustrous, black cannel, from Stony Creek. 2. Dull, earthy canuel, from Hartley. 3. Brown, lustrous cannel, from Lower Hunton. 4. Bright cannel. from Colley Creek. 5. Dull, earthy, carbonaceous shale, from Illawarra. 6. Brownish lignite, from Barra- gomerg. Accompanying them are some fossils of Palaeozoic type. 272. Coal from Bosewood, Kendal county, Queensland. Of Carboniferous age. Analysed by W. J. Ward. Carbon - - 68-28 Hydrogen - 6-34 Oxygen and Nitrogen - -9-08 Sulphur - O40 Ash (pale red)- - 13-98 Water - - 1-92 100-00 48 See Percy's Metallurgy, Fuel, p, 343. A massive, lignite-like, dull coal, yielding 50-35 per cent, of firm lustrous coke. 273. Coal from Flagstone Creek, Queensland. Of Carboni- ferous age. Analysed by W. J. Ward. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash (white) Water - 100-00 See Percy's Metallurgy, Fuel, p. 343. A moderately tender, irregularly banded coal, yielding 66-36 per cent, of firm lustrous coke. Communicated by E. Daintree. 274. " Allora " coal, Queensland ; of Carboniferous age. Analysed by W. J. Ward. Carbon - 69-31 Hydrogen - - 6*08 Oxygen and Nitrogen - - 11-51 Sulphur - - 0-31 Ash (buff) - 8-87 Water - - - - 3-92 100-00 A compact, rather dull, feebly banded coal, yielding 70- 16 per cent, of coke and 25-92 per cent, of volatile matter. .Communicated by E. Daintree, 1873. 275. " Thomas " coal, Queensland ; of Carboniferous age. Analysed by W. J. Ward. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash (white) Water - 100-00 A bright coal, with irregular fracture, yielding 72 50 per cent, of coke and 25*59 per cent, of volatile matter. Communicated by R. Daintree, 1873. 276. " Davies " coal, Queensland ; of Carboniferous age. Carbon - 79-01 Hydrogen - 5-19 Oxygen and Nitrogen - -6-56 49 Sulphur - - 0-37 Ash (pale red) - - - 7-73 Water- - 1-14 100-00 A not brilliant, compact, and rather thin-banded coal, yielding 68 84 per cent, of coke and 30*02 per cent, of volatile matter. Communicated by E. Daintree, 1873. 277. Coal from New South Wales, imported in 1872. A tender coal, with variable bands. Of probably Carboniferous age. 278. Coal from New South Wales, imported in 1872. A dull, thin-banded, compact coal. Both these coals were imported in H.M.S. " Eclipse " and communi- cated by the Sheerhess officers. Dr. Percy gives (Metallurgy, Fuel, p. 344) two analyses of coals from this locality, but it is not indicated which of these correspond to either. They are I. II. Carbon - 77 '65 65 '11 Hydrogen - 4 '94 4 '61 Oxygen and Nitrogen - 1 63 1 1 93 Sulphur - 0-58 0'68 Ash - - 3-25 7'12 Water - - - 2 -95 10.55 100-00 100-00 279. " Bulli " coal, Cumberland county, New South Wales ; of Carboniferous age. Analysed by W. J. Ward. Carbon - 75-57 Hydrogen - 4-70 Oxygen and Nitrogen - 4*99 Sulphur - ' 54 Ash - - - 13.17 Water- - - 1-03 100-00 See Percy's Metallurgy, Fuel, p. 344. A dull, tender coal, with broad bands, yielding 74-78 per cent, of coke. 280. Coal from New South Wales, Of Carboniferous age. See " See Mines and Mineral Statistics of New South Wales," 1875.. Bituminous coal from a ten foot seam. Australian Agricultural Com- pany's Colliery, Newcastle. An excellent house, steam, gas, smelting, and caking coal. Brilliant, compact, scarcely banded. Communicated by J. Mackenzie, 1873. 281. Coal from New South Wales. Of Carboniferous age. Bituminous coal from a ten feet seam. Lambton Colliery, near Newcastle. An excellent house, steam, gas, smelting, and caking U 61955. 50 coal. Bright, compact, and banded. Communicated by J. Mackenzie, 1873. 282. Coal from New South Wales. Of Carboniferous age. Bituminous coal from a ten feet seam. Waratah Colliery, near Newcastle. An excellent house, steam, gas, smelting, and caking coal. Moderately 'bright, compact, and banded. Communicated by J. Mackenzie, 1873. 283. Coal from New South Wales. Of Carboniferous age. Bituminous coal from the Dukinfield Colliery, near Newcastle. An excellent house, gas, steam, smelting, and caking coal. Compact, fairly bright, broad banded. Communicated by J. Mackenzie, 1873. 284. Coal from New South Wales. Of Carboniferous age. Semi-bituminous coal from a ten feet seam. From the Bulli Colliery, near Wollongong, An excellent steam, smelting, and house coal. Dull, feebly banded, small splintering. Communicated by J. Mackenzie, 1873. 285. Coal from New South Wales. Of Carboniferous age. Splint coal from a 26 foot seam. Greta Colliery, 35 miles from Newcastle. This seam of coal has 1 ft. of Boghead cannel in it. An excellent gas, steam, smelting, house, and coking coal. Bright, very compact, fine banded. Communicated by J. Mackenzie, 1873. 286. Coal from New South Wales. Of Carboniferous age. Splint coal from a 10 ft. 6 in. seam. In the Upper Coal Measures, Lithgow Valley, County Cork. This seam is worked by the Bowenfels, Lithgow, Esk Bank, and Vale of Clwydd Colliery Companies. Very dull, compact, feebly banded. Communicated by J. Mackenzie, 1873. 287. Coal from Cape Paterson, near Victoria, New South Wales. Sent by A. Burrell. Analyses are given by Dr. Percy, Metallurgy, Fuel, p. 344, of two samples of coal from this locality ; but there is no indication as to which of these two specimens corresponds to the two analyses made by C. Tookey. They are - Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - Water - 100-00 100-00 Of these two samples, one is more compact, regularly banded, and dull the other, more irregular, thinner banded, and brighter. 288. New Zealand coal. Bituminous non-caking coal from Bninner Mine, Nelson. From the exhibits of the Colonial Museum in the Vienna Exhibition, 1873. 51 Much jointed, homogeneous, tender and friable ; lustre pitch-like, glistening ; often iridescent ; colour black, with a purple hue ; powder, brownish ; cakes strongly ; the best varieties forming a vitreous coke with brilliant metallic lustre ; average evaporative power 74 Ibs. of water per Ib. of coal. Occurs with grits and conglomerates of Upper Neocomian age in seams' 2 to 20 ft. in thickness. 289. New Zealand coal. Semi-bituminous coal from Pre- servation Inlet, Otago. From the exhibits of the Colonial Museum in the Vienna Exhibition, 1873. Compact with laminae of bright and* dull coal alternately; fracture ir- regular ; lustre moderate ; cakes moderately, or is non-caking ; rarely cakes strongly; evaporative power 6J Ibs. Occurs in thin irregular seams in sandstone of Upper Neocomian age. 290. New Zealand coal. Glance coal from Hills Drive, Malvern Hills, Selwyn, Canterbury. From the exhibits of the Colonial Museum in the Vienna Exhibition, 1873. Non-caking, massive, compact, or friable ; fracture cuboidal, splintery ; lustre glistening to metallic ; structure obviously laminated ; colour black ; does not form a compact coke, but slightly adheres. A variety of brown coal altered by faults or igneous rocks, and presenting every intermediate stage from brown coal to an anthracite. 291. New Zealand coal. Pitch coal from Shag Point, Otago. From the exhibits of the Colonial Museum in the Vienna Exhi- bition, 1873. Of compact structure ; fracture, smooth, conchoidal ; jointed in large angular pieces; colour brown or black; lustre waxy; does not desiccate much on exposure, nor is it absorbent of water ; burns freely, and contains resin distributed throughout its mass. Evaporative power 4*2 Ibs. Derived from beds of Upper Neocomian age. 292. New Zealand coal. Brown coal from Saddle Hill Otago. From the exhibits of the Colonial Museum in the Vienna Exhibition, 1873. Barely shows vegetable structure ; fracture irregular, conchoidal, with incipient laminations; colour dark brown ; lustre feeble; cracks readily on exposure to atmosphere, losing 5 to 10 per cent, of water, which is not reabsorbed ; burns slowly ; contains resin in large masses. Evaporative power 5 Ibs. From the lower part of beds of Upper Neoeomian age. 293. Coal from the West Coast of the Middle Island, New Zealand. Analysed by C. Tookey. Of supposed Miocene age. Carbon - 79-00 Hydrogen - 5-35 Oxygen - 7-71 , Nitrogen - 0-89 Sulphur 2 '50 Ash - - - - 3-50 Water - - 1 05 100-00 D 2 52 See Percy's Metallurgy, Fuel, p. 344. Irregular, dull, small splintering coal, yielding 64 -82 per cent, of coke. Communicated by C. L. Carter. 294. Coal from Kawa-Kawa, Auckland, New Zealand. Bitu- minous coal ; of Tertiary age. Contains Combustible matter - - 88-48 Sulphur - 5-42 Ash - - 1-70 Water - - - - -4-40 100-00 A dull, resinous looking coal, yielding 57 per cent, of coke. One ton occupies one cubic yard. Communicated by the Colonial Museum, New- Zealand, 1868. 295. Coal from Grey River, Westland, New Zealand. Bitu- minous coal ; of Tertiary age. Contains Combustible matter - - 91 '81 Ash - - 6-20 Water- - 1-99 100-00 A bright, broad-banded, compact coal, yielding 68 7 per cent, of coke.. One ton occupies -999 cubic yards. Communicated by the Colonial Museum, New Zealand, 1868. 296. Coal from Buller River, Coalbrookdale, Nelson, New Zealand. "Nine-foot seam" of bituminous coal; of Tertiary age. Contains Combustible matter - -95-80 Sulphur - 1-20 Ash - 40 Water- - 2-60 100-00 A rather bright, very compact coal, yielding 65 8 per cent, of coke- One ton occupies 1*066 cubic yards. Communicated by the Colonial Museum, New Zealand, 1868. 297. Coal from Pakawan, Nelson, New Zealand. " Seven- foot " seam of bituminous coal ; of Tertiary age. Contains Combustible matter - - 87-14 Sulphur - - 1-04 Ash - - - 8-26 Water - - 3.56 100*00 53 A rather dull, very compact coal, with bright bands, yielding 58 8 per cent, of coke. One ton occupies "909 cubic yards. Communicated by the Colonial Museum, New Zealand, 1868. 298. Cool from Acvere River, Nelson, New Zealand, A " one-foot " seam of bituminous coal ; of Tertiary age. Contains Combustible matter - - 94-00 Ash - 3-80 Water - 2-20 100-00 A moderately dull, very compact, banded coal, yielding 58-5 per cent, of coke. Communicated by the Colonial Museum, New Zealand, 1868. AFRICAN COALS. 299. Coal from Stormberg, Cape of Good Hope. Of Carbon- iferous age. Analysed by W. J. Ward. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - Water - 100-00 See Percy's Metallurgy, Fuel, p. 340. A bright, compact coal, with almost a conchoidal fracture, and yielding 67-88 per cent, of coke. See Dunn, Quart. Journ. Geol. Soc., vol. 27. Also Report on Storm- berg Coalfield. Communicated by the Crown Agents, 1871. 300. Coal from Transvaal. Probably of Carboniferous age. Heavy, dull, and compact, very feebly banded. 301. Coal from Zambesi river, discovered by Dr. Livingstone. See " Expedition to the Zambesi and its Tributaries," 1865. Analysed by W. J. Yv r ard. Carbon Hydrogen Oxygen and Nitrogen - Sulphur Ash - - - Water - 100-00 A compact, dull, irregularly banded coal, partly in loose particles, Communicated by the Admiralty. 54 302. Mineral found in the hills distant not more than 30 miles inland from Machinga Bay on the Zanzibar coast, a little t > the south of Keleva. Found in 1878. Analysed by W. J. Ward. Carbon - 58 67 Hydrogen - 4 ' 57 Oxygen and Nitrogen - - - 12*73 Sulphur - - 1-58 Ash - - 1-45 Water- - - - - 21-00 100*00 A compact cannel coal, resembling Wigan cannel, with a bright con- choidal fracture. Communicated by Dr. Kirk. 303. Coal from the Camdeboo Mountains, South Africa. Of Carboniferous age. (See E. J. Dunn's "Keport on the Camdeboo and Nieuwveldt Ccal," Cape of Good Hope, 1879.) The coal called " Vices," middle portion, yields 19 per cent, of ash ; 2-40 per cent, of water ; 1-25 per cent, of sulphur ; and 64 per cent, of fair coke. It is compact, dull, and narrow banded. Collected by E. J. Dunn. 304. Coal from Camdeboo Mountains, South Africa. Of Carboniferous age. (See 303.) "Vices " coal, bottom portion. Yields 17-80 per cent, of ash ; 2 per cent, of water ; 1 per cent, of sulphur ; and 64 per cent, of fair coke. It is dull, compact, with narrow, bright bands. Collected by E. J. Dunn. 305. Coal from Camdeboo Mountains, South Africa. Of Carboniferous age. " Hal tings " coal, middle portion. Yields 29 per cent, of ash ; 90 per cent, of water ; 84 per cent, of sulphur. It is compact, tender, and banded alternately bright and dull, and an imperfectly caking coal. Collected by E. J. Dunn. 306. Coal from Camdeboo Mountains, South Africa. Of Carboniferous age. " Haltings " coal, bottom portion. Yields 24 per cent, of ash ; 1 -0 per cent, of water ; 1 .05 per cent, of sulphur. It is a rather tender ,nd thin banded non-caking coal. Collected by E. J. Dunn. 307. Coal from "" November Kraal, Cape Colony." Yields 23-60 per cent, of ash; 1*30 per cent, of water ; 1-05 per cent, of sulphur. It is a tender, bright banded, non-caking coal. Collected by E. J. Dunn. 308. " Dundee " coal, from Natal. A banded bituminous coal. Communicated by Ar. Browning. 55 COKES. 309. Hair-like coke. Produced by a bubble of hydrocarbon vapour being more highly heated, and decomposing, depositing its carbon on the surface ; two such bubbles adjacent to each other build up thus a wall between them ; and three produce a narrow thread standing out from the surface of the coke. See Percy's Metallurgy, Fuel, p. 421. 310. No. 1 Glamorgan coke. 311. No. 2 Glamorgan coke. 312. No. 3 Glamorgan coke. 313. Foundry coke. Newton, Chambers, and Co, 314. Coke used at the Tonddu Iron Works. Made from No. 3 coal. Mailts Moel Colliery, Ogmore Valley, near Bridgend, Glamorganshire. 315. Rhondda coke, in small fragments. 316. Anthracite coke. Made in an ordinary beehive oven by the Bouvilles Court Coal and Iron Company, Saundersfoot, S. Wales. The ingredients used were anthracite slack, 70 ; bituminous slack, 25 ; and pitch, 5 per cent. A very brilliant but irregular coke. 317. Anthracite coke, made in an ordinary beehive oven, at the Kilgetty works of the Borwelle's Court Coal and Iron Company, 1873. The ingredients used were, anthracite slack, 25 ; and bituminous or caking slack, 75 per cent. Less brilliant and irregular. 318. " Lowry " or " Parkend " coal, in the Forest of Dean and the coke that is made from it. This is the only kind in use at the Cinderford furnaces (1875). See No. 170. The coal is bright and slightly banded, the coke is pretty compact. 319. Coke used at the Parkend furnaces, Forest of Dean, made from the "Lowry" or "Parkend" High Delf coal. 320. Light coke, from the South Staffordshire thick coal. Used in the blast furnaces, Russell's Hall, Dudley. 321. Medium coke from the South Staffordshire thick coal. Used in the furnaces at Russell's Hall, Dudley. 322. Heavy coke from the South Staffordshire thick coal, Russell's Hall, Dudley. A very dense and lustrous coke, capable of bearing a heavy burden. 56 323. Slack coke made from the South Staffordshire ten yard or thick coal, Dudley. In small pieces. Communicated by S. Blackwell. 324. Coke produced by a mixture of equal weights of pitch and the slack of South Staffordshire thick coal. (1859.) Coked in Jones' coke oven, at the Russell's Hall Furnaces, Dudley, of which a full description is given in Percy's Metallurgy, Fuel, p. 438. The resulting coke is used in the blastfurnaces. It is dull and very regularly scoriaceous. Communicated l?y S. Blackwell. 325. Light coke from the Heathen coal. South Staffordshire, Russell's Hall, Dudley. 326. Coke from Peareth gas coal. Made by exposing the pulverised coal to a dull red heat in a Stour- bridge clay crucible, until the evolution of gas ceased. 327. Two samples of coke from Peareth gas coal. Prepared at a low temperature, by exposing the finely pulverised coal to a full red heat for about three-quarters of an hour, and increasing the heat for a few minutes. The crucible was embedded in a second pot filled with anthracite, to exclude air. Experiment byR. Smith. (1856.) In one of these samples the pulverised coal was inserted dry ; in the other it was previously wetted and rammed in. 328. Coke from Peareth gas coal. Prepared at a high temperature by exposing the finely pulverised coal to a bright red heat for about an hour, the crucible being embedded in anthracite. In one of the two samples the powder was dry; in the other it was wetted with water and well rammed down in the crucible. Experiment by R. Smith. (1856.) 329. Coke from an old gas retort at Leith, near Edinburgh. (1840.) Showing a laminated structure, and of a highly specific gravity. 330. Coke from steam coal obtained at Seaton Burn Colliery, near Newcastle-on Tyne. (1856.) Produced by exposing the pulverised coal to a dull red heat in a covered Stourbridge clay pot until evolution of gas ceased ; time about 1 hour. 331. Coke from the Abercarn Black Vein steam coal, Newport, Monmouthshire. Analysed by E. Jackson. Carbon Hydrogen Oxygen and Nitrogen - Ash - 100-00 Contains 0-45 per cent, of moisture and 0-75 per cent, of sulphur. 57 332. Coke produced from the Tertiary lignite of Bovey Tracey, Devonshire, without pulverisation. Very light and charcoal-like. 333. Coke prepared at a high temperature from the " White " coal, Whyley Pit, South Staffordshire. The very finely powdered coal was .placed in a covered Cornish crucible, enclosed in a Stourbridge clay pot, filled up with anthracite powder to exclude the air. It was then heated as rapidly as possible at a strong red heat for rather more than half an hour. This coke shows well the arborescent and mammilated form produced on the surface by the rapid and irregular evolution of gas. A little further subdivision would produce the hair-like coke, No. 309. 334. Coke prepared as 324 5 part, in fact, of the same preparation. And showing a quantity of hair-like coke in the crevices where the main mass has separated, the crevices being closed at the surface and wider below. One of these is filled, not with round hairs, but with th'in plates. A finely laminated coke. 335. Result of heating pulverised " Thick coal " in a furnace for half an hour, the temperature being raised as rapidly as possible. Forms a pulverulent and scarcely coherent coke. Experiment by E. Smith. (1855.) 336. Patent coke. From the Glamorgan Coal Company, South Wales, No. 1. Analysed by W. J. Ward. (1878.) Carbon - 85-73 Hydrogen - 0-73 Oxygen and Nitrogen - 0-88 Sulphur - 0-74 Ash - 8-08 Water - -3-84 100-00 A very porous coke. Communicated by W. Perch and Co. 337. Patent coke from the Glamorgan Coal Co., South Wales, No. 2. Analysed by W. J. Ward. Carbon - 92-73 Hydrogen - 0-64 Oxygen and Nitrogen - -0-60 Sulphur - 0-79 Ash - - 4-87 Water - - 0-37 100-00 58 338. Coke used for iron smelting at the Dunbar Ironworks, Pennsylvania. A strong lustrous coke. Analysed by Mr. Habrishaw. It contains Carbon - - - - 89-047 Volatile matter - 1 296 Sulphur - 0-184 Water at 125 C. - 0-032 Ash - - - 9-523 100-032 The ash is composed of silica 5-413, alumina 3272, ferric oxide 0-479, lime 0-243, and phosphoric acid 0-012. 339. Coke produced from the slack of the Main Seam Albion Mines, Pictou County, Nova Scotia. Communicated by G. M. Dawson. PATENT FUELS. 340. Dawson's Patent Fuel. Produced by the subjection of coal slack to heat and pressure. (1851.) 341. Portion of the fuel which oozes out from the iron box during the process of compressing the slack in Dawson's patent process. 342. The coal powder which is moistened with water and afterwards subjected to heat and compression in the manufacture of patent fuel by Dawson's process. (1856.) 343. Venallt Patent Fuel, South Wales. Made by compressing slack combined with a bituminous substance. Communicated by Wm. Gregory. 344. Patent fuel in cylinders made by the compression of slack. Four samples. 1. Suitable for locomotives and steamships. 2. From steam coal. 3. From anthracite. 4. From bituminous coal. 345. Mineral charcoal. Two samples from different coals. It is light and porous and easily broken. Used as a substitute for wood-charcoal in the manufacture of tin-plate iron. The coal is powdered and washed and spread in its wet state over the floor of a reverberatory furnace previously heated to redness. Much ebullition and evolution of gas occurs and the residue in about an hour is the mineral charcoal. 346. Samples of Barker's Patent Fuel. Produced by mixing fragments of coke or coal with farinaceous matter, and subjecting them to compression. No. 1 is made from coke. 59 No. 2 is the same material which has been re-coked in an oven. No. 3 is made from " Nixon's Navigation " coal. No. 4 from Powell's Duffryn coal; and No. 5 from Lambton's Wallsend. REFRACTORY MATERIALS FOR FURNACES, &c. CLAYS, BRICKS, AND SANDSTONES. 347. Stannington fire-clay. From carboniferous beds in the Sheffield District. It is used for cast-steel pots. After desiccation its analysis gives : Silica - Alumina Earths and Alkalies Iron Oxide - - - Water in combination - 99-76 See Percy's Metallurgy, Fuel, Ac., p. 98. 348. Edgemount pot-clay. From carboniferous beds near Sheffield. Used in making crucibles for melting cast-steel. Its analysis by W. J. Ward, after desiccation, gives : Silica - - - - - 45-73 Alumina - - 34-14 Alkalies and Earths - 1-98 Iron Oxide - - - -1-76 Water combined - 10-17 Water hygroscopic "- 4-45 Organic matter - 0-70 98-93 See Percy's Metallurgy, Fuel, &c., p. 98. Communicated by Mi. 3. Morgan. It is accompanied by samples ground and burnt. 349. Fire-clay from Edensor. From carboniferous beds near Derby, Used in making crucibles for cast-steel. After desiccation its analysis gives : Silica - - - - - 48-08 Alumina - 36-89 Alkalies and Earths - 2-43 Iron Oxide - 2-26 Water combined - 10-87 100-53 See Percy's Metallurgy, Fuel, &c., p. 98. 60 350. Carboniferous fire-clay from Buckley Mountain, Flint- shire. The lowest bed and best quality worked. Burns white, and is largely used for fire-bricks at the Holywell Lead Furnaces and at Swansea. 351. Teignmouth clay, Devonshire, known as the chocolate variety. It is used as an ingredient in JulefFs crucibles. It really occurs at Bovey Tracey, but is called Teignmouth clay from its port of .shipment. It is a white Tertiary clay, and its analysis by W. Weston gives : Silica - - 52-06 Alumina - 29-38 Alkalies and Earths - . - 2-74 Iron Oxide - ,. - 2-37 Water combined 10-27 Organic matter , - traces. Water hygroscopic - -2-56 99-38 See Percy's Metallurgy, Fuel, &c., p. 99. 352. Clay from Poole, Dorsetshire. A white Tertiary clay used as an ingredient in Juleft's crucibles. Its analysis gives : Silica - Alumina - - . - Alkalies and Earths - Iron Oxide - , - - Water combined Water hygroscopic 99-36 See Percy's Metallurgy, Fuel, &c., p. 99. 353. China clay from South Cornwall Mining Company's Works. It is a white clay derived from the decay of the neighbouring granite. Analysed by W. J. Ward, after desiccation. Silica - - 47-75 Alumina - - - 38-11 Alkalies and Earths - 0-91 Iron Oxide - - - 0-69 Water combined - - 12-54 100-00 See Percy's Metallurgy, Fuel, &c., p. 100. 354. Fire-clay from the Star Fire-brick Works, Glenborg, near Coat Bridge, N.B. 61 Used for fire-bricks, Bessemer tuyeres, &c. A dark, carbonaceous, hard, sandy clay. Communicated by J. Dunnackie. 355. Black Stourbridge fire-clay, used for making " London pots '' by the Patent Plumbago Crucible Company, Batfcersea. A carboniferous under-clay. 356. French fire-clay, 'used in making French crucibles by the Patent Plumbago Crucible Company, Battersea. See Percy's Metallurgy, Fuel, &c., p. 121. A sandy loose clay. 357. White Stourbridge- fire-clay, used for making "Glass pots " by the Patent Plumbago Crucible Company, Battersea. A strong brown sandstone. Communicated by Mr. Gadby. 358. Red clay, Devonshire. Analysed by W. J. Ward. Silica - - 57-83 Alumina - 20-55 Ferric Oxidte - - 7-75 Manganous Oxide - trace. Lime - Potash Soda - Carbonic Acid - Phosphoric Acid Water combined Water hygroscopic 100-63 In its moist state it contained 24-42 per cent, of water. A uniform red clay apparently derived by weathering from the Trias clays. 359. Belgian clay, imported into Swansea for zinc retorts. See Percy's Metallurgy, Fuel, p. 122. A soft grey clay. 360. " China stone " from the Isle of Man. A white siliceous material used for brick-making for furnaces, from the ancient schists of the island. A portion of it tested in a crucible by Mr. R. Smith accompanies the mass. Communicated by A. Klingenden. 361. Sand as occurring at S. Agnes Beacon, Cornwall. One of the ingredients of Juleffs Cornish crucibles. Communicated by Mr. Gadby. 362. Prepared composition of JulefFs Cornish crucibles Kedruth. It consists of one part of Teignmouth clay (No. 351), one part of Poole clay (No. 352), and two parts of sand from S. Agnes Beacon, Cornwall (361), all by measure, and is yellowish white and granular. See Percy's Metallurgy, Fuel, p. 118. Communicated by Mr* Gadby. 62 363. China stone from Cornwall. A. green siliceous stone, accompanied by specimens of the result of fusing it in a platinum crucible. 364. Result of trials with Glascote fire-clay, from near Tamworth. See Percy's Metallurgy, Fuels, &c., p. 99. It is cut into trial pieces of the form described and figured, loc. cit., p. 113. 365. Tested clays from the Rockingham Clay Works, West Willow, Romsey, Hants. White uniform clays. Communicated by Mr. Sturgeon. 366. Fire-clay from Way Wood, with the results of testing the same. A hard, micaceous, gritty, banded rock. Communicated by Mr. Dougall Smith. 367. The original rock from whence is derived the material for the (< Dinas fire-bricks." A very hard, compact, siliceous rock, found at Dinas, in the Vale of Neath, Glamorganshire. Too hard to be worked by itself. Analysed by W. Weston. Communicated by E. Young. Silica - - - - 96-73 Alumina - 1-39 Iron Oxide - 0-48 Lime - 0-19 Alkalies - 0-20 Water combined - 0-50 99-49 See Percy's Metallurgy, Fuels, &c., p. 147. . 368. The weathered material actually used for the Dinas bricks. It occurs in the soft, crumbly state, as well as in the condition of hard rock, but the latter is known to become softer by weathering. 369. The prepared material used for the manufacture of Dinas bricks, consisting of the rock ground with one per cent. of lime. . See Percy's Metallurgy, Fuel, &c., p. 147. 370. The varieties of material required for the manufacture of Devonshire fire-bricks. They are all derived from the decomposition of granite, and for use the best composition is found to be one part of " coarse mica " and two parts of" fine sand.'* The several varieties are as follows : 1. " Coarse sand." This consists of the larger masses of quartz which are separated from the kaolin used for china clay. 2. " Fine sand." This consists of the finer particles of quartz, mixed with much of the mica, and a small proportion of some more basic ingredient of dark tint. 3. " Pipe 63 clay." This is the separated kaolin. 4. " Coarse mica." This consists of the kaolin mixed with the larger fragments of partially decomposed mica. 5. " Fine mica." This consists of the kaolin mixed with the finer fragments of the mica. 371. Soft, white, friable, siliceous material between Great and Little Ormes Head, near Llandudno. Suitable, when mixed with a little clay, for furnaces and the setting of fire-bricks, but used also for building and shipped as ballast. 372. Aluminous mineral from Ireland (? from Belfast). With results of testing it (1) by heating alone, (2) by mixing it with 10 per cent, of French fire-clay, (3) by mixing it with 20 per cent, of French fire-clay. 373. Fragments of the Pennant grit rock, a coarse sand- stone belonging to the Coal Measure series, which have been built into the Gwyther Old Furnace, South Wales, and have, there- fore, long been subjected to heat, of which the effects may be seen in the specimens. 374. Sandstone used for hearth stone in the Glyndon Furnace on the river Lehigh, Easton, Carbon County, Pennsyl- vania, U.S.A. A coarse siliceous grit. 375. Columnar structure produced at Glyndon Furnace, Lehigh River, Pennsylvania. This is formed at the mouth of the furnace, of the sandy loam used in closing up the outlet after casting. It is black and hard, but com- paratively light. 376. Samples of Dinas fire-bricks. The fracture is very rough, owing to the irregular white particles of quartz which are set in a yellowish matrix. 377. Material of which the Dowlais fire-brick is made. It is known as the " Little Vein West Clay." Analysed when burnt into brick by E. Eiley, and yields : Silica - Alumina Earth and Alkalies Iron Oxide - Titanic Acid - 99-92 See Percy's Metallurgy, Fuel, &c., p. 150. 378. Sample of material and results of experiments on " Windsor bricks." These bricks are red, and known as PP. fire-bricks, and are made at Chalfont St. Peters, Buckinghamshire, The material is a soft, red, 64 argillaceous sandstone. See Percy's Metallurgy, Fuel, p. 150, where an analysis is given. 379. Buckley fire-brick, used for lead smelting furnaces. From Buckley, in Flintshire ; a specimen brought from the Dee Bank Lead Works. It is a very coarse yellowish red brick, with particles of unaltered white silica ; also used for parts exposed to great heat in chimneys, flues, &c. See Percy's Metallurgy, Fuels, &c., p. 150, where an analysis is given. 380. Stormy fire-brick ; formerly used as a substitute for Dinas bricks. This is a siliceous brick made from boulders scattered over Lias- Limestone, near Bridge End. Pyle, Glamorganshire. These were collected and ground, but the manufacture has been discontinued as too expensive, and the resulting brick too tender. 381. A portion of brick made by the Chinese on the Bendigo- Gold Fields. They take the clay and knead it with " sludge," mould it into bricks and bur them in a kiln, somewhat resembling a conical coke oven, but very large. About half-way up the interior of the kiln are four openings for piping, one and a half inch diameter, through which they force water by means of a pump. The bricks are carefully packed so as to let as much surface as possible come in contact with the hot air and steam. 382. Fragment of reddish white fire-brick from India; together with the results obtained by R. Smith in testing its- power of resisting fusion, showing it to fuse slightly. Communicated by H. Bauerman. 383. Sand as used for beds of copper furnaces. 384. Tanners spent bark, burnt into ashes, and sieved ready for mixing in water with which to wash the inside of copper cake moulds. 385. Ganister used for furnace bottoms. From the quarry at Hazlehead, near Penistone. Communicated by Sir J. Brown and Company. 386. Gornal sandstone altered by heat. From the hearth of the blast furnace, Woodside. It has become roughly columnar in structure with slickensides. Communicated by A. B. Boden. 387. Specimen showing the action of silicate of iron upon a Cornish crucible. It has invaded the substance of the crucible and divided it into- numerous irregular lamella, which are filled with the melted substance in a glassy form. 65 388. Specimen showing the action of. oxide of iron on a tire- brick of interior quality from Sielce. It has entered into combination, and is commencing to perforate the brick. GRAPHITE. 389. Natural graphite from Ceylon. As used by the Patent Plumbago Crucible Company in making " black-lead" crucibles. It is very massive, with a fibrous striation. 390. Native graphite from the Horicon Mines, Triconderoga, on Lake Champlain, U.S.A. The mass is divided into bands from f to f inch in thickness, and the finer foliaB of graphite cross these bands obliquely, and at different -angles in different bands. 391. Native graphite from the Horicon Mines, Triconderoga. Showing a crystalline or, platy form. It is very irregular, and apparently from a disturbed mass. 392. Native graphite from the Horicon Mines, Triconderoga. Showing a massive form, with an indefinite number of fine bands of irregular form, each of which is , produced by very fine transverse, crystalline plates set side by side. These three samples are all from the " Laurentian" rocks of the State of New York, where they occur in bauds. 393. Sample of purified graphite from Horicon Mines, Tri- conderoga. This is called "Photographers' graphite," and is purified first mechani- cally, and then chemically, so that the remaining impurity does not exceed 5 per cent. From the American Graphite Company, New York. 394. Sample of purified graphite from Horicon Mines, Tri- -conderoga. This is called " Electrotypers' graphite," and is purified by mechanical means only. From the American Graphite Company, New York. 395. Specimen of the material used in making the Morgan crucibles. This has been tested in the Metallurgical Laboratory of the Royal School of Mines by incineration in a muffle heated to whiteness, and it has yielded 51-66 per cent, of a yellowish- white residue, giving 48-34 per cent, of graphite. See Percy's Metallurgy, Fuel, &c., p. 126. 396. Plumbaginous or graphitic anthracite from the mica schists of Worcester, 45 miles west of Boston, U.S.A. Brought by Sir Chas. Lyell. Analysed by Dr. Percy. U 63.955. v. 66 Carbon - - - - 28-350 Hydrogen - 0-926 Oxygen and Nitrogen - -2-155 Ash - - - 68-569 100-000 A well-banded mass very graphitic in appearance. See Quart, Journ. Geol. Soc., vol. I., p. 205. CASTING MATERIALS, &c. 397. Casting sand from Birmingham. A fine red sand from below the Bunter series. It- takes a sharp mould. Communicated by J. P. Marrian. 398. Casting sand from Japan. From a core in which it had been used. Analysed by W. J. Ward, including the fragments of charcoal with which it is mixed. Silica - Alumina Iron Oxides - Oxides of Copper, Zinc, and Manganese Earths and Alkalies - Sulphuric Acid Carbon - Water - 99-78 See Percy's Metallurgy, Fuel, &c., p. 153. Communicated by J. Fisher. 399. Substance of the mould used for large steel castings at Messrs. Spear and Jackson's Atlas Works, Sheffield, 1885. It is very hard and dark grey, and seems to contain much graphite, but its actual composition is not stated. 400. Loam used for casting moulds and cores at the Wool- wich Arsenal. COPPER. EXPERIMENTS SHOWING THE PROPERTIES OF COPPER. 401. Copper scale. Consists almost wholly of copper dioxide. It is largely produced in the process of annealing sheet copper in rolling mills, with access of air. See Percy's Metallurgy, 1861, p. 242. 402. Pulverized copper scab 67 403. Copper scale heated to redness with access of air, and thereby converted into cupric oxide. 404. Cuprous oxide, produced by heating cupric oxide with copper. A hard red mass of artificial cuprite, an important ore of copper. 405. Cuprous oxide, produced by heating one equivalent of copper sulphide with two equivalents of copper sulphate at a low heat in a covered pot. 200 grains of copper sulphide and 400 grains' of copper sulphate were taken. Experiment by W. Baker, 1854. 406. Cuprous oxide, produced by heating one equivalent of cuprous sulphide with four of cupric sulphate. 300 grains of copper sulphide with 1,200 grains of cupric sulphate were heated together in a covered pot to a low red heat. Experiment by W. Baker. 407. Cuprous oxide, produced by heating five equivalents of cuprous chloride and three of sodium carbonate, and digesting the product in water. 408. Cupric oxide exposed to a high temperature. It has melted to' a purple slag-like mass. 409. Result of heating silica with cuprous oxide in the pro- portion of 30 to 70, or 3 Cu 2 O, 2 Si0 2 . Conducted by R. Smith. The mixture was heated strongly in a plumbago crucible. The pro- duct was fritted, but not melted, and forms a hard earthy red mass. See Percy's Metallurgy, 1861, p. 243. 410. Result of heating silica with cupric oxide in the proportion of 84 : 116, or CuO, Si0 2 . Conducted by R. Smith. This was exposed to an intense heat in a French pot for about two hours. This only partially softened, but did not entirely fuse the mixture, producing an earthy, irregular, black and red banded mass. See Percy's Metallurgy, 1861, p. 244. 411. Result of heating silica with cupric oxide in the pro- portion of 44 : 58, or 3 CuO, 2 SiO 2 . Conducted by R. Smith. The materials were intimately mixed, and the mixture exposed in an uncovered platinum dish to a strong red heat in a muffle during 3 J hours, about half the product was again exposed during 5J hours to a heat approaching whiteness. No perceptible change occurred. The results of both are here. They are dark earthy masses with a red fracture. See Percy's Metallurgy, vol. I., p. 244. 412. Bisulphide of copper. Produced by the direct combination of flowers of sulphur with copper scale. It is black, with fine radiating crystals from the sides of the crucible. E 2 68 413. Result of the experiment of heating cuprous oxide with iron bisulphide and sUica. 1,296 grains of cuprous oxide wore mixed with 786 grains of bisulphide of iron and 276 grains of silica, and heated in a plumbago crucible with charcoal. The result is threefold : at the top is a smooth compact slag, in the middle is a regulus-like bisulphide of copper showing a little moss-copper here and there, and a button of copper through which bisulphide of copper is diffused. Experiment by B. Smith, 1856. See Percy's Metallurgy, 1861, p. 2o5. 414. Bisulphide of copper. Produced by fusing six equivalents of cupric oxide, six of pyrites, and , two of silica. Yielding two of silicate of iron and six of bisulphide of copper. A steel-grey mass of metallic lustre. 415. Copper bisulphide coating the surface of copper foil. Produced by leaving the foil in a flask with flowers of sulphur at the ordinary temperature of the air for some days, whereby it has become quite black by being covered by a loose layer of sulphide. 416. Copper bisulphide. Produced by heating together copper wire and sulphur in a flask. The form of the fragments of copper wire is not lost, but they are con- verted nearly or quite to, the centre into the above-named black com- pound. 417. Artificial copper pyrites. , Produced by fusing copper bisulphide with two equivalents of iron bisulphide or native iron pyrites. Two atoms of sulphur are expelled, leaving a double sulphide of the formula Cu 2 S -f 2 FeS containing by analysis 30-39 per cent, of sulphur. 1,000 grains of Cu 2 S and 1.513 of FeS 2 were taken. It is of a dull brass yellow colour. Experi- ment by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 217. 418. Artificial copper pyrites. Producad by fusing together copper bisulphide with two equivalents of iron sulphide, adding sulphur in pieces and stirring with a woodon rod. 1,000 grains of Cu 2 S and 1,109 grains of FeS were taken, and the analysis of the product gave sulphur 29-6 per cent. The formula Cu 2 S-|-2FeS corresponds to 28-69 per cent, of sulphur, showing that no more was taken into composition. Experiment by W. Baker. See Percy's Metallurgy, 1861, p. 247. 419. Massive bisulphide of copper. Artificial copper-glance, consisting of dull black square prisms one inch in the side. 420. Artificial copper pyrites. Produced by fusing together one equivalent of copper bisulphide and one of iron sulphide. 320 grains of the former and 176 grains of the latter were token and fused in a covered crucible, producing 450 grains of pyrites, much resembling the "blue-metal" of copper smelters. See Percy's Metallurgy, 1861, p. 247. 69 421. Artificial bisulphide of copper. Produced by fusing copper scrap and sulphur on a large scale (30 Ibs.). It shows crystals arranged in an arborescent form, and having a brassy lustre. Experiment by W. RatclifFe, Wolverhampton, 1876. 422. Copper produced by mixing copper bisulphide with two equivalents of cuprous oxide. There were heated together in a luted pot for 25 minutes at a strong red heat 1,000 grains of Cu 2 S and 1,796 grains of Cu 2 O. The copper obtained weighs 2,301 grains. Experiment conducted by W. Baker, 1 854. See Percy's Metallurgy, 1 86 1 , p. 250. 423. Copper produced by mixing copper bisulphide with two equivalents of cupric oxide. 1,000 graius of each ingredient were taken and heated together in a luted pot at a strong red heat. The button of copper weighed 1,295 grains. Experiment conducted by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 250. 424. Copper produced by mixing one equivalent of copper bisulphide with one of copper sulphate. 500 grains of each were taken and heated in a luted crucible for 25 minutes at a strong red heat. The button of copper weighed 516 grains. Experiment conducted by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 250. 425. Kesult of experiment to show the action of silica in melting copper bisulphides in an earthen crucible. One equivalent of copper bisulphide and four of copper sulphate were mixed and heated at a regulated temperature until converted entirely into cupric oxide. The heat was then increased, and the oxide of copper combined with the silica contained in the pot, forming A very fusible silicate. This v as poured out into a mould, forming a dark brown massive substance (here broken in two), and a portion of the corroded pot preserved, showing an irregular black surface and discoloured section. Experiment conducted by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 250. 426. Result of heating four equivalents of copper with one of protoxide of lead. 320 grains of granulated copper were fused with 280 grains of litharge, the resulting metallic button weighed 340 grains, and was accompanied by a red -brown slag. It contained 308-4 grains, or 90 '7 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 250. 427. Result of heating two equivalents of copper with one of protoxide of lead. 320 grains of copper and 560 grains of protoxide of lead were fused together, and the product consisted of 340 grains of red mortal accom- panied by a red brown glassy slag. 70 428. Result of heating one equivalent of copper with one of protoxide of lead. 320 grains of copper and 1,120 grains of litharge were fused together, and the product consisted of 321 grains of metal and of red-brown slag. The button contained 233 7 grains, or 72 8 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 251. 429. Result of heating one equivalent of copper with two of protoxide of lead. 320 grains of copper and 2,240 grains of litharge were fused together and a button of metal weighing 392 grains was obtained, and in a second experiment when the copper was granulated, 373 grains, accom- panied by a mottled slag. The button, in the last case, contained 203 9 f rains, or 54 66 per cent, of copper. Experiment by R. Smith. See ercy's Metallurgy, 1861, p. 251. 430. Result of heating one equivalent of copper with three of protoxide of lead. 160 grains of copper and 1,680 grains of litharge were fused together, and a button of metal weighing 195 grains was obtained. The slag shows two layers, the upper one rich in copper, the lower one rich in lead. The button contained 56-9 grains, or 29-2 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 251. 431. Result of heating one equivalent of copper with six of protoxide of lead. 64 grains of copper and 1,344 grains of litharge were fused together, and a button of metal weighing 86 grains was obtained. The slag is dark brown and vitreous. The button resembled lead, and contained 10-6 grains, or 12-3 per cent, of copper. Experiment by R, Smith. See Percy's Metallurgy, 1861, p. 251. 432. Result of heating two equivalents of copper and one of sulphate of lead. 320 grains of copper and 760 grains of lead sulphate were heated together. The reaction only takes place at a strong red heat. The slag produced is dark and scoriaceous on the surface, and brick red below. Two globules of copper weighing 11 ! grains were left. Ex- periment by E. Smith. See Percy's Metallurgy, 1861, p. 252. 433. Result of heating one equivalent of copper with one of sulphate of lead. 160 grains of copper and 760 grains of lead sulphate were heated together. There were no globules of copper, and the slag weighed 640 grains. It is brownish red, with a darker and sub-metallic surface. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 252. 434. Result of heating two equivalents of cupric oxide with one of metallic lead. 800 grains of the cupric oxide and 1,040 grains of granulated lead were fused together, yielding a crystalline black slag with semi-metallic lustre, I&periment by R. Smith. See Percy's Metallurgy, 1861, p. 253. 71 435. Result of heating three equivalents of cupric oxide and two of metallic lead. 480 grains of cupric oxide and 832 grains of lead were fused together. The resulting metallic button weighed 460 grains, and contained 330-7 grains, or 71*9 per cent, of copper. The slag is reddish brown, and semi-vitreous. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 253. 436. Result of heating one equivalent of cupric oxide with one of metallic lead. 400 grains of cupric oxide and 1,040 grains of lead were fused together. The resulting metallic button weighed 343 grains. The experiment was repeated on half the above quantities, and the metallic button weighing 180 grains contained 119-7 grains, or 66 '5 per cent, of copper. The slag is reddish brown. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 253. 437. Result of heating one equivalent of cupric oxide with two of metallic lead. 200 grains of cupric oxide were fused with 1,040 grains of lead. The resulting button weighed 574 grains, consisting of lead mixed with copper. It is accompanied by a black, highly vitreous slag, which is reddish brown in thin flakes. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 253. 438. Result of heating one equivalent of cuprous oxide with one equivalent of oxide of lead. 720 grains of copper scale and 1,120 grains of litharge were fused together at a low red heat, producing this dark crystalline mass. It shows signs of contraction on cooling. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 253. 439. Result of heating one equivalent of cuprous oxide with two of oxide of lead. 720 grains of cuprous oxide were fused with 2,240 grains of litharge. Produces a similar dark crystalline mass, the upper coat of sub-metallic lustre, but no lead is formed. The mass has a contraction cavity in the centre. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 253. 440. Result of heating one equivalent of cupric oxide with one of oxide of lead. 400 grains of cupric oxide were heated with 1,120 of litharge. The result is a hard dark crystalline slag. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 253. ' 441. Result of heating one equivalent of cupric oxide with two of oxide of lead. 200 grains of cupric oxide were fused with 1,120 grains of litharge. The result is a dark greenish slag, with radiating crystallisation and hollow centre. Experiment by R. Smith. See Percy's Metallurgy 1861, p. 253. 442. Result of heating one equivalent of cupric oxide with one of lead sulphide. 400 grains of cupric oxide were fused with 1,200 grains of pure galena, and produced a button of regulus weighing 705 grains, together with a black vitreous slag. The experiment was repeated with half quantities, and the button weighing 302 grains, yielded 142-3 grains, or 47 '15 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 254. 443. Result of heating three equivalents of cupric oxide with two of lead sulphide. 600 grains of cupric oxide were fused with 1,200 grains of galena, and produced a regulus weighing 710 grains, with a button of metal below. It contained 504 grains, or 71 '04 per cent, of copper. There is also a vitreous brown-red slag. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 254. 444. Result of heating two equivalents of cupric oxide with one of lead sulphide. 800 grains of cupric oxide were fused with 1,200 grains of galena, and produced a regulus with a copper-coloured button at the bottom. The whole weighed 565 grains, of which the button was 307 grains, con- taining 299 grains, or 97 4 per cent, of copper. The slag is a hard sealing- wax-red opaque glass. Experiment by R. Smith. See Percy's Metal- lurgy, 1861, p. 254. 445. Result of heating three equivalents of cupric oxide with one of lead sulphide. 1,000 grains each of cupric oxide and galena were fused together, and produced a brownish-red slag, with a button of metal weighing 140 grains, of which 138-6 grains, or 99 per cent., is copper ; the slag only is here. Experiment byR. Smith. See Percy's Metallurgy* 1861, p. 254. 446. Result of heating four equivalents of cupric oxide with one of lead sulphide. 800 grains of cupric of oxide were fused with 600 grains of galena, and produced a red opaque slag and a copper-like button weighing 162 grains, and containing 156-7 grains, or 96-7 per cent, of copper; the slag only is here. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 254. 447. Result of heating sulphide of copper with carbon. 200 grains of copper sulphide were exposed to a high temperature in a brasqued crucible, and produced 8 5 grains of metallic copper, with 189-5 grains of unchanged sulphide. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 257. 448. Result of heating one equivalent of sulphide of copper with one of iron. 1,000 grains of copper sulphide were fused with 353 grains of iron filings in a crucible with a luted cover, for about 20 minutes at a strong red heat, and produced a regulus and a button of metal weighing 853 grains. This button, analysed by Mr. Tween, gave copper 62-45, 73 iron 31-70, and sulphur 3-85 per cent. Experiment by W. Baker. See Percy's Metallurgy, 1861, p. 257. 449. Result of heating one equivalent of sulphide of copper with two of iron. 1,000 grains of copper sulphide and 700 grains of iron filings were fused together, and produce4 a brittle crystalline regulus of iron-grey colour. Experiment by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 257. 450. Result of heating two equivalents of sulphide of copper with one of iron. 1,000 grains of copper sulphide were fused with 910 grains of iron in a luted crucible and anthracite fire for 45 minutes, and produced a purple-coloured regulus and no metal. Experiment by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 257. 451. Yellow copper ore fused and stirred with metallic iron. This illustrates the statement (Percy's Metallurgy, 1861, p. 258) that metallic iron exerts little reducing effect upon .the double sulphide of copper and iron, the result being still the compound sulphide, rather browner and dark in the middle by the introduction of a larger propor- tion of iron. 452. Result of heating one equivalent of sulphide of copper with four of iron. 1,000 grains of copper sulphide were fused with 1,410 grains of iron filings in a luted pot with anthracite for 45 minutes, and produced a dark grey regulus, which is crystalline, except its upper layer, and transfused in it is a certain amount of moss-copper, and a few crystals like those of copper sulphide. Experiment by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 258. 453. Result of heating one equivalent of copper sulphide with one of zinc. 320 grains of copper sulphide were fused with 128 grains of zinc in fine powder in a luted crucible at a bright red heat for 20 minutes, and the result weighed 246 grains. It consists of a thin layer of bluish-grey regulus and a metallic button-like brass ; the regulus contains 58-4 per cent, and the button 81 -8 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 258. 454. Result of heating one equivalent of copper sulphide with two of zinc. 160 grains of copper sulphide were fused with 128 grains of zinc at a bright red heat ; the result weighed 182 grains, consisting of a layer of regulus weighing 119 grains, and a button of metal weighing 63 grains. The regulus has its upper surface partially covered with moss-copper, and contains 62-37 per cent, of copper. The button contains 80-9 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 258. 455. Result of heating one equivalent of copper sulphide with one of lead. 74 400 grains of copper sulphide were fused with 520 grains of finely granulated lead in an unluted crucible. The result is a dark grey regulus, and a button of malleable metal weighing 495 grains, of which 10 -3 per cent, is copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 258. 456. Result of heating two equivalents of copper sulphide with three of lead. 400 grains of copper sulphide were fused with 780 grains of lead, and the result is a dark grey regulus, and a button of malleable metal weigh- ing 753 grains and containing 8-84 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 259. 457. Result of heating one equivalent of copper sulphide and two of lead. 400 grains of copper sulphide were fused with 1,040 grains of lead, and the button of metal produced weighed 1,019 grains, containing 6*76 per cent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 259. 458. Result of heating one equivalent of copper sulphide and one of tin. 1,000 grains of copper sulphide were fused with 741-7 grains of tin in powder. They were placed in a luted pot and heated to bright redness for 10 minutes. The product is a grey regulus containing tin, and a white metallic button having the composition, tin 65-17, copper 33-25, sulphur 0-37 per cent. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 259. 459. Result of heating one equivalent of copper sulphide and one of antimony. 160 grains of copper sulphide and 258 grains of antimony were fused together, and produced a regulus containing 57 48 per cent, of copper, and a metallic button like antimony, containing 19-2 percent, of copper. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 260. 460. Result of heating three equivalents of copper sulphide and one of antimony. 240 grains of copper sulphide and 129 grains of antimony were fused together, and produced a regulus containing 57 9 per cent, of copper, and a button of metal containing copper 33-40, antimony 60-56, and sulphur 6-04 per cent. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 260. 461. Result of heating three equivalents of copper with one of tersulphide of antimony. 192 grains of copper wire in small pieces were fused with 354 grains of tersulphide of antimony at a bright red heat for half an hour in a luted crucible. The product is regulus and metal, of which the former con- tains 47-53 per cent, and the latter 3-86 per cent, of copper. Experi- ment by W. Baker. See Percy's Metallurgy, 1861, p. 260. 462. Result of heating six equivalents of copper with one of tersulphide of antimony. 75 380 grains of copper were fused with 354 grains of antimony ter- sulpliide, and produced a regulus containing 66-44 per cent., and a button of metal containing 42 54 per cent, of copper. Experiment by W. Baker. See Percy's Metallurgy, 1861, p. 26 1/ 463. Result of heating 12 equivalents of copper with one of tersulphide of antimony. 761 grains of copper were fused with 354 grains of antimony ter- sulphide. and produced a regulus containing 75 9 per cent., and a button of metal containing 66*72 per cent, of copper. Experiment by W, Baker. See Percy's Metallurgy, 1861, p. 261. 464. Eesult of heating 18 equivalents of copper with one of tersulphide of antimony. 1,141 grains of copper were fused with 354 grains of antimony ter- sulphide, and produced a regulus containing 77 '36 per cent., and a button of metal containing 75 90 per cent, of copper. Experiment by W. Baker. See Percy's Metallurgy, 1861, p. 261. 465. Result of heating bisulphide of copper with 25 times Its weight of litharge. 100 grains of copper sulphide were fused with 2,500 grains of oxide of lead, and produced a button of metal resembling lead, weighing 422 grains, and 21-67 grains of copper adhering as a film to the surface of the button. This amount of litharge is therefore more than enough to oxidise all the sulphur. Experiment by W. Baker, 1854. See Percy's Metallurgy, 1861, p. 262. 466. Result of heating three equivalents of copper with one of tersulphide of antimony. 190 grains of copper were heated with 354 grains of tersulphide of antimony, and the result as seen was a button of metal containing antimony 95-97, copper 3-86, sulphur 0-17, and a regulus contain- ing copper 47-53, antimony 29-32, sulphur 23*15. Experiment by Ambrose Tween. See Percy's Metallurgy, 1861, p. 260. 467. Result of heating one equivalent of silver sulphide with two of cupric oxide. A button of copper and silver is produced. 468. Artificial oxychloride of copper. Strips of copper foil were put into a wide-mouthed bottle and kept moistened with strong hydrochloric acid, diluted with its own volume of water. The bottle was closed with a loose fitting cork, kept in a warm place and shaken from time, to time. This oxychloride was thus produced. Analysed by R. Smith. Copper - 59-24 Chlorine ~ 16-87 Oxygen - 11-15 Water by difference - - - 12-74 100-00 Corresponding to the formula CuCl 2 , 3 CuO, 3 H 2 O. See Percy's Metallurgy, Silver and Gold, p. 78. 76 469. Experimental liquation of lead from copper. Stage 1. By heating the mass to the fusing point of copper and letting it gradually cool ? It shows a thick covering of copper on the surface of the lead. 470. Experimental liquation of lead from copper. Stnge 2. It shows a thin covering of copper on the surface of the lead. ' 471. Liquated copper and liquation cake. The copper contained 2*2 per cent, of silver, and was melted with three parts of common lead. Accompanying these is a sample of the grey coating on the surface of the lead and copper alloy. 472. Result of experiment on roasted pyrites with lead. 2,000 grains of roasted pyrites from California, 850 grains of silica, 750 grains of lime, 38 grains of charcoal, and 500 grains of lead were melted together. The result consists of a small non-sectile metallic button floating in a large sectile button, the whole being covered by a green glassy slag, with white fragments scattered in it irregularly. Experiment by R. Smith. 473. Result of experiment on roasted pyrites and lead. 1,000 grains of roasted pyrites from California were heated with the same weights of silicn, lime, charcoal, and lead as in the last experiment. The result is Very similar, the non-sectile hutton is absent. Experiment by R. Smith. 474. Metallic copper as a red-coloured powder, precipitated by heating solutions of copper sulphate and sugar together. Experiment by R. Smith. 475. Copper precipitated by zinc. From a solution of sulphate of copper, acidulated by hydrochloric acid. Experiment by W. Baker. It is in the form of a black powder. 476. Copper precipitated by iron from a solution of copper sulphate. As a black powder. 477. Copper prepared from copper scale. By digesting it in dilute sulphuric acid and washing the residue till free from the copper sulphate formed. A black powder. Experiment by W. Baker. 478. Copper prepared from copper scale by hydrogen. A copper-coloured powder. 479. Copper containing phosphorus. Made by heating copper in a mixture of bone ash and charcoal in a charcoal crucible to a white heat for about an hour. Experiment by A. Dick. See Percy's Metallurgy, 1861, p. 281. It consists of dark grey globules of various sizes, from a mustard seed downwards. 77 480. Phosphide of copper obtained by the reduction of copper phosphate by carbon. 860 grains of copper phosphate was heated with 240 grains of char- coal af a strong red heat. A dark grey metallic button weighing 200 grains was obtained. Experiment by K. Smith. See Percy's Metallurgy, 1861, p. 280. 481. Phosphide of copper by the reduction of copper phos- phate by carbon, starch and carbonate of soda. 1,000 grains of phosphate of copper, 200 grains of charcoal, and 500 grains each of starch and carbonate of soda were heated together at a strong red heat; the resulting carbonaceous mass with metallic globules was again heated with 500 more grains of carbonate of soda, and a dark grey button weighing 210 grains is the result. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 280. 482. Phosphide of copper cast at Chatham. Employed for copper refining by Weston's process. Accompanied by the small masses of metal that ooze out of the surface during the process ; a reddish-grey metallic mass. 483. Result of experiment with copper zinc and sodium in 1858. 200 grains of finely powdered zinc, 200 grains of copper foil cut in pieces, and 200 groins of sodium cut in pieces were heated in 600 grains of silico-fluoride of potassium. The result is a yellowish-white metallic button weighing 268 grain?, and a quantity of grey opaque glassy slag. 484. Arsenide of copper. 500 grains of copper, 500 grains of starch, and 1,000 grains each of ursenious acid and carbonate of soda were heated together at a strong red heat. The dark grey crystalline metallic button weighed 760 grains, and was accompanied by a little black slag. Experiment by II. Smith. See Percy's Metallurgy, 1861, p. 281. 485. Alloy of silicon and copper. Produced in Cowles' electric furnace. This has been remelted and cast into an ingot. The silicon in com- bination has been reduced from pure white sand by means of a strong current of electricity passed from large carbon po'es through the mix- ture. The alloy contains 10*59 per cent, of silicon and 89*41 per cent, of copper. The value of this alloy lies in the combination of great tensile strength with great conductivity. Thus while pure copper requires a breaking weight of 17 '78 tons per square inch, in this silicon copper, commonly called silicon bronze, the breaking weight is 28*57 per square inch, while the conductivity is only decreased 4 per a," 1863. Communicated by J. Nicholson. SPECIAL APPLICATIONS OF COPPER. 1217. Glass coloured with red oxide of copper. It shows a beautifully crystalline structure under the microscope. It is manufactured near St. Petersburg. Specimens were exhibited in the Exhibition of 1862. There is a fine specimen in the Slade Collection in the British Museum. 151 1218. Opaque glass filled with minute separate copper scales, giving it a red colour. Communicated by Mr. Matthews. 1219. Glass coloured red by copper oxide. Perfectly transparent. 1220. Glass " flashed " with a fine layer of copper glass. From Messrs. Chance's Works, Birmingham. The copper glass is opaque at a distance, the red colour by reflected light preventing the passage of the transmitted light, which is seen to be green when the glass is held to the light. 1221. Copper deposited in the interior of an incandescent lamp. A fifty-candle Edison lamp. It very rarely happens that such a copper deposit is formed. The copper is vaporised when the greatest resistance in the circuit happens to be at the copper junction of the carbon film and platinum wire. This lamp shows the vertical line of no deposit, or shadow of the carbon film which indicates that the particles of* copper are ejected in straight lines from the heated junction. The deposited copper when thin enough is seen to be green by transmitted Jight. See Fleming, Phil. Mag., July 1883, p. 48. Communicated by him. 1222. Glass containing oxides of copper and iron. The tear-like piece shows two colours, the one red, produced by gently heating and slowly cooling, the other green, produced by strongly heating and rapidly cooling. See Percy's Metallurgy, 1861, p. 351. ZINC. EXPERIMENTS. 1223. Result of heating one equivalent of zinc with two of litharge. 160 grains of zinc in fine powder were heated with 1,120 grains of litharge, in a well- covered clay crucible to a strong red heat Tor three quarters of an hour. The result is a button of malleable lead, weighing 245 grains, and an imperfectly fused slag of dark brown colour. 1224. Result of heating together two equivalents of zinc and one of galena. An imperfectly metallic porous mass, not thoroughly fused. 1225. Zinc heated with phosphorus. Said to give it a more silver-like colour. 1226. Result of heating one equivalent of zinc oxide with one of boracic acid. 20C grains of zinc oxide were fused with 175 grains of boracic acid in a platinum crucible, to strong redness in a muffle for half an hour, 152 arid poured into an open ingot mould. The result is a colourless trans- parent glass, slightly opalescent on the surface, with conchoidal, non-crystalline fracture. See Percy's Metallurgy, 1861, p. 538. 1227. Result of heating two equivalents of zinc oxide with one of boracic acid. 240 grains of zinc oxide were fused with 105 grains of boracic acid in the same manner as the last. The result is a white, vitreous, crystalline, translucent solid, with a large lamellar fracture and pearly lustre. See Percy's Metallurgy, 1861, p. 538. 1228. Result of heating three equivalents of zinc oxide with one of boracic acid. 240 grains of zinc oxide were fused with 70 grains of boracic acid in the same manner as before. The result is vitreous, pale yellow, and opaque in mass, but translucent in small pieces. The fracture is less largely lamellar, and the lustre less pearly. See Percy's Metallurgy, 1861, p. 538. 1229. Result of heating three equivalents of oxide of zinc "with two of boracic acid. 240 grains of oxide of zinc were fused with 140 grains of boracic acid in the same manner as before. The result is a beautiful transparent glass, with no trace of crystallisation. Experiments by R. Smith. See Percy's Metallurgy, 1861, p. 538. 1230. Result of heating one equivalent of zinc oxide with one of silica. 200 grains of zinc oxide were heated with 230 grains of fine Australian sand of great purity, in a Cornish crucible placed in a muffle during five hours to a strong heat at or near whiteness. The product is fritted only and not melted. See Percy's Metallurgy, 1861, p. 536. 1231. Result of heating two equivalents of zinc oxide with one of silica. 240 grains of zinc oxide were heated with 138 grains of the same sand, under the same conditions as the last. The product is fritted, but not so firmly as the last. See Percy's Metallurgy, 1861, p. 536. 1232. Result of heating three equivalents of zinc oxide with one of silica. 240 grains of zinc oxide were heated with 92 grains of the same sand, under the same conditions as before. The product is fritted more than the last. See Percy's Metallurgy, 1861, p. 536. Experiments by R. Smith. 1233. Result of heating together four equivalents of zinc and one of arsenic. 132 grains of zinc were heated with 75 grains of arsenic in a glass test tube. They combined with a red glow at a temperature considerably below a red heat, forming a porous mass of peculiar fracture and sub- metallic lustre. It was not changed by subjecting it to a good red heat in a covered crucible, but at a bright red heat was volatilised. See Percy's Metallurgy, 1861, p. 547. 153 1234. Result of heating zinc with 10 per cent, of arsenic. This produces no glow when heated, but the result has a similar fracture, rather more coherent. See Percy's Metallurgy, 1861, p. 547. 1235. Zinc and arsenic. Result of stirring pulverised arsenic with melted zinc. One portion remained fluid in the centre, the remainder became a very porous solid mass. Samples of both are here. The solid portion is crystalline, so that an arsenide of zinc appears to be formed. Experiment by R. Smith. 1236. Zinc and arsenic. A hard scum of peculiar bluish lustre, and smelling strongly of arsenic. 1237. Crystals obtained by exposing zinc oxide and zinc sulphide to a white heat in a Cornish crucible. They are minute, obscure, brownish-yellow crystals incrusting the crucible. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 541. 123S. Zinc oxide heated with alumina on platinum foil. One equivalent of ziuc oxide was mixed with six equivalents of anhydrous alumina in a small crucible of platinum foil, enclosed in a covered and luted clay crucible. It was heated for an hour in Deville's furnace ; the result is a compact, grey, stony substance which scratches glass. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 539. 1239. Result of heating zinc oxide in a blende-lined crucible. The clay crucible was filled with Laxey blende in powder solidly rammed down, closed with well-luted covers, and strongly heated for half an hour. A cavity was made in the blende, thus firmly aggluti- nated, and 40 grains of zinc oxide were inserted and the remainder filled with powdered blende. The crucible was enclosed in a plumbago crucible, and heated to white heat for an hour. The cavity which had been filled with zinc oxide is now quite empty, the blende is much acted on here, and the clay crucible below the cavity is coloured blue. The cover of the clay crucible is coated with small brown crystals. Experi- ment by R. Smith. See Percy's Metallurgy, 1861, p. 542. 1240. Result of heating a mixture of zinc oxide and zinc sulphide in a blende-lined crucible. 20 grains of oxide of zinc were intimately mixed with 92 grains df Laxey blende, i.e. in the ratio of one equivalent of zinc oxide to three of zinc sulphide. The mixture was treated in the same way as in No. 1239. A light porous crystalline residue (contained in the glass-capped box) was found in the blende cavity. This is the weight that ought to be left if the zinc oxide and sulphide combined to form zinc and sulphurous acid. Experiment by R. Smith. See Percy's MetaUurgy, 1861, p. 542. 1241. Result of heating zinc oxide and zinc sulphide in a blende-lined crucible. 40 grains of zinc oxide were mixed with 48 grains of zinc sulphide, i.e. in the ratio of one equivalent of zinc oxide to one of zinc sulphide, 154 and treated in the same way as in No. 1239. A light porous residue weighing 22 grains is left, the proper balance from the reaction being 24 grains. The crucible cover is again lined with brown crystals. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 542. 1242. Result of exposing sulphide of zinc to a high tempera- ture. 200 grains of Laxey blende free from matrix were very strongly heated in a small Stourbridge clay crucible in Deville's furnace during JJ hours, with anthracite. The crucible was covered with various other crucibles. The blende has become firmly agglutinated, though not fused, into one mass, and has lost nine grains in weight. On the upper part of the crucible is seen some dark crystalline matter of a somewhat metallic lustre. Experiment by R. Smith. Sec Percy's Metallurgy, 1861, p. 540. 1243. Result of heating sulphide of zinc with tin. 96 grains of pulverised Laxey blende and 116 grains of granulated tin were exposed together in a covered clay crucible to a bright red heat during half an hour. A metallic button weighing 14-5 grains has been produced. It is harder than tin, but has been flattened considerably under the hammer, but not without slightly cracking at the edges. Its fracture is crystalline-granular, and it has nearly the colour of tin, but contains zinc. This is covered by an easily separable regulus weighing 11 grainy. It is hard, brittle, finely granular in fracture, and iron-grey in colour. The internal surface of the crucible is not acted on, nor is it permeated. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 543. 1244. Result of heating sulphide of zinc with antimony. A mixture of 144 grains of Laxey blende and 120 grains of antimony was prepared by trituration, and exposed in a covered clay crucible to a bright red heat during half an hour. The product consists of an aggluti- nated and firmly coherent mass weighing 245 grains, thereby showing a loss of 19 grains ; it is easily fractured, and shows a uniform mixture of particles of blende and a well-melted metal resembling antimony ; in certain lights a cleavage with a brillant metallic lustre is shown. Ex- periment by R. Smith. See Percy's Metallurgy, 1861, p. 543. 1245. Result of heating sulphide of zinc with lead. A mixture of 192 grains of pulverised Laxey blende and 416 of finely granulated lead was exposed in a covered clay crucible, at a bright red heat during three quarters of an hour. The product is an imperfectly fused cavernous mass, hard, brittle, largely crystalline, dark lead-grey, and metallic in lustre. The internal surface of the crucible has been acted on and covered with a brown porous substance. No metallic lead is seen. Experiment by R. Smith. See Percy's Metallurgy, 1861, p. 543. 1246. Result of heating sulphide of zinc with copper. A mixture of 48 grains of Laxey blende with 128 grains of powdered copper was exposed in a covered clay crucible to a bright red heat during half an hour. The product consists of a button of metal and regulus. The metal resembles brass in colour and fracture, and weighs 85 grains. The regulus resembles sulphide of copper, and weighs 155 71 grains. This shows a reduction of the zinc. Experiment by B. Smith. See Percy's Metallurgy, 1861, p. 544. 1247. Fragments of crucibles used in the above experiments. They show crystals in various spots. 1248. Result of heating oxide of zinc with iron. 80 grains of zinc oxide were intimately mixed with 56 grains of iron wire in very small pieces, and heated in a wrought-iron crucible at a very high temperature for one hour within a French pot. The result is a mass of iron and a black glassy slag. In the exterior crucible is a dark green glass, as if the wrought-iron pot had leaked. Experiment by B. Smith. See Percy's Metallurgy, 1851, p. 536. 1249. Result of fusing together three equivalents of silicate of zinc of the formula 3 ZnO . Si0 2 , with one equivalent of borate of zinc of the formula 3 ZnO . BO 3 , in a platinum crucible at a white heat. This is equivalent to introducing 5 -37 per cent, of boracic acid. One result is a translucent greenish- white glass. ZINC ORES. 1250. Laxey blende. The sulphide of zinc, obtained at Laxey, and used at Hafod. Pounded to small fragments. 1251. Calami ne or carbonate of zinc, in a transparent crystal- line form. 1252. Calamine from Sweden. As used at the Vieille Montagne Works, Belgium, for the manufac- ture of Belgian zinc. In a brown, earthy form, 1253. Silicate of zinc. From Bethlehem, Pennsylvania, U.S.A. In a stalactitic form. 1254. Artificial blende or sulphide of zinc. From the Muldner Hutte, Freiberg. An incrustation on the surface of the roasting furnaces. 1255. Franklinite, an oxide of zinc, iron, and manganese. From New Jersey Mining Company, Newark. Communicated by H. Bauerman. After calcination it is treated as an iron ore. 1256. Franklinite, from New Jersey. An oxide of zinc, iron, and manganese. Used first for the extraction of zinc, and the residue smelted for manganiferous iron. 156 PRODUCTS OF THE OPERATIONS FOR THE EXTRACTION OF ZlNC. 1257. Calcined blende mixed with coke ready for distillation. Vivian's Works, 1848 In small fragments. 1258. Calcined blende, without coke. Vivian's Works, 1848. In small fragments. 1259. Calcined calamine. From Llansamlet Spelter Works, Swansea, 1869. The inner part has an incrustation of rhombic white crystals, which are radially- arranged about numerous points. 1260. Incrustation on the inner surface of the top of Silesian zinc pot. This is an arborescent yellow mass of crystalline oxide of zinc. One specimen shows brilliant crystal faces. Communicated by Messrs. Dillwyn, 1859. 1261. Fragment of zinc pot, from an old English zinc furnace. From Mines Royal Works, 1869. Shows a scoriaceous scum on the surface of the blue-purple pot, which is coated with a fused brown substance within. 1262. Concretion of oxide of zinc formed by leaving the pot in the furnace. A curved shell-like mass of consolidated powder of white oxide, showing a radiating and concentric structure, coated with loose powder within. Communicated by Mr. Clifford, Fazeley Street Mills, Birming- ham. 1263. Zinc from the internal surface of a condensing tube in the English process. Vivian's Works, Morriston, Swansea, 1848. 1264. Piece of spelter pot, impregnated with zinc and thus rendered purple to a certain depth. This will be used over again wish fresh Stourbridge clay in making new pots. 1265. Piece of old spelter pot, impregnated with zinc and associated substances. It looks purple and scoriaceous. 1266. Portion of an old Belgian zinc retort. Used at the Spelter Works, Dee Bank. Showing two layers ; the inner the edge of the fused contents, the outer the impregnated pot of purple colour with unaltered, siliceous fragments. 1267. Microscopic section of a Silesian zinc retort, from Lipine, Silesia. 157 Showing the formation of zinc spinel. See Freiberg Jahrbuck, 1881. Communicated by H. Bauerman. 1268. Mammillated crystalline zinc oxide. From the bottom of a spelter pot at Mines Royal Works, 1859, where spelter was then obtained by the English process. Communicated by W. Edmonds. 1269. Zinc oxide incrustation, as a greenish- white crystalline stalactite. From the New Jersey White Zinc Works. See Am. Journ. Sci., Fol. 13, p. 417. 1270. Powdered oxide of zinc. From Hafod Zinc Works, 1848. This is produced in the Silesian and Belgian processes. See Percy's Metallurgy, 1861, p. 586. 1271. " Grey oxide of zinc." Collected from the neck of the retorts at Alston Works. Com- municated by G. Attwood. 1272. Zinc fume. From the Alston Works. Contains 49 92 of zinc. Communicated by G. Attwood. 1273. Tube of oxide of zinc formed on a cupel in which zinc was heated in a muffle. Produced at the Metallurgical Laboratory, Jermyn Street, 1880. The cupel on which it was formed accompanies it. It has a very close resemblance to a long coral from the chalk, possessing both longitudinal furrows and transverse lines of growth. The furrows, however, some- times bifurcate and sometimes reunite. The tube is quite hollow, and has a crater-like top, free from any radial grooves. 1274. Zinc fumes, called " Blue oxide." From Vivian's Spelter Works, Morriston, Swansea, 1883. Contains zinc in a finely divided state, mixed with its oxide. 1275. Consolidated zinc fumes, from the Zinc Works of Laurium, Greece. Showing columnar formation. Grey oxide within coated with white oxide. 1276. Consolidated zinc fumes from Laurium, Greece. Showing a fine and contorted columnar formation. Grey oxide coated with white oxide. 1277. Scoria from the distillation of zinc. Hafod Zinc Works, 1848. 1278. Residium of the zinc pots. Vivian's Works, Swansea. An earthy, dark, crumbling mass. 158 1279. Refuse from the spelter pot. After the zinc has been distilled away, all the non-volatile material in the ore or in the coke is left as an open mass in the bottom of the pot. This is chiefly derived from the triturated ore. It is fragmontal in structure. 1280. Slag from spelter pot. This is another variety of the same refuse derived more directly from the fuel. It resembles a purple coke. 1281. Spelter dross. Heated to a very high temperature in an open pot, then with a perforated ladle the sediment is removed from the bottom of the pot. Rylands' Works, Warrington. A mass of grey metallic crystals of prismatic form. Communicated by F. Dixon. 1282. Spelter dross. The refuse of the hard spelter, after it has been in a closed pot and heated so high as to drive off all the spelter. It is a mass of beautiful iridescent grey, rhombic metallic crystals. Mostly of prismatic form. Communicated by F. Dixon. 1283. Crystallised zinc oxide. From the New Jersey, U.S.A., White Zinc Works. From Professor G. J. Brush, Yale College. Long, greenish, transparent needles. 1284. Iridescent crystals in zinc. Formed on heating zinc which had been accidentally mixed with dross and refuse in the ash-pit. Ry lands' Works, Warrington. These are very like the crystals of No. 1282. Communicated by F, Dixon, 1873. METALLIC ZINC. 1285. Zinc made from silicate ores. Minerva Works, Wrexham. It is very tough, and not so bright as that made from blende or oxide ores, but the grain is good. Communi- cated by G. Darlington. 1286. Zinc produced by the old English process. Hafod Works, Swansea, 1848. Largely crystallised. 1287. Zinc from the Warrington Galvanising Works. Bank Quay, Warrington, 1873. Very brilliant narrow crystals* Communicated by F. Dixon. 1288. Sheet zinc rolled cold. 1289. Finely granulated zinc. 1290. Zinc showing a very large crystalline cleavage. Communicated by C. Tookev. 159 1291. Sample of zinc showing a finely lamellar crystalline fracture. Communicated by F. A. Dixon. Warrington, 1873. 1292. Zinc melted at a low temperature under carbon, and cooled slowly. It is a granular mass, but each granule is globular and smooth, and more or less adherent to the neighbouring ones, the whole formiug an, arborescent pseudo-crystallisation. 1293. Hollow conical forms of zinc. Produced by dropping melted zinc into water. The cones have undulating surfaces. 1294. Commercial zinc recrystallised. The zinc has been melted in an earthen pot, and allowed to cool slightly ; then the surface broken and the still fluid contents in the- centre poured out. 1295. Zinc containing T46 per cent, of lead. Communicated by Muntz and Co. 1296. Impure zinc. Contains 0' 1 7 per cent, of iron, and 1 '26 per cent, of lead. Analysis by R. Smith. Communicated by Muntz and Co. 1297. Zinc free from arsenic. 1298. Zinc specially prepared pure. By the chemiot at the works of Messrs. Rylunds Brothers, Warring- ton. Shows a broad and brilliant cleavage. 1299. Zinc perfectly free from iron. Prepared by R. Smith. Analysed by C. Tookey. 1300. Zinc redistilled and free from iron. 1301. An ingot of the first zinc produced in Finland. Produced from Finnish ore the original silver-lead-zinc blende, by means of wood, turf and sawdust as fuel. Made by Finnish workmen in part, at Arainne, Pojo, south coast of Finland, the only spelter works in North-East Europe, 1879. Communicated by Mr. Julin. 1302. Chinese zinc from the province of Yunan. Brought by Sir Harry Parkes. The fracture is platy, but very irregular and spotted. 1303. Zinc which has been in a steam boiler for six weeks. At the Rhys Las Works, Dowlai?, South Wales. It is now entirely brittle, and has for the most part been converted into red oxide, the innermost parts only being grey. 1304. Samples of manufactured zinc. Perforated examples. 160 1305. Samples of zinc tubing with galvanised iron roofing. Communicated by F. Braby. ALLOYS OF ZINC. 1306. Zinc containing sodium. Tt has been fused at a low temperature, in an iron crucible under salt. It has a whiter, more compact, and granular fracture than zinc alone. 1307. Alloy of two equivalents of zinc with one of tin. 1,475 grains of tin were fused with 1,622 grains of zinc; the com- pound has therefore 52 '42 per cent, of zinc. It has a brilliant platy fracture. 1308. Alloy composed of one equivalent of antimony to three of zinc. It has been melted in a crucible to which it firmly adheres. It has a brilliant bluish-white fracture, soon tarnishing, but not crystalline. The surface has numerous crystalline plates crossing each other. Two specimens. Communicated by Mr. Keats, of Bagillt Lead Works. 1309. Pump-barrel metal. Consisting of 44 parts of zinc, 44 of tin, and 12 of antimony per cent. The fracture is small and granular, with occasional small flakes. 1310. Zinc and lead, Commercial zinc melted with about 2 per cent, of lead, well stirred and cooled rapidly by removing the crucible and its contents from the furnace and plunging it into cold water. The lead does not mix, but is found collected at the lower surface. Experiment by E. Smith, 1856. 1311. Alloy of zinc and antimony. Fused in a crucible. Made by Professor Josiah Cooke, Junior, of Harvard College, Cambridge, U.S.A., in the laboratory of the Royal School of Mines, It adheres to the sides of the crucible as a solid metallic mass below, its surface having large long dull iridescent crystals in form like antimony. 1312. Alloy of 96 ! per cent, of zinc, and 2*6 per cent, of iron. Has a curious laminated transverse fracture. 1313. Alloy of zinc and iron from Gospel Oak Works, Staffordshire. Remelted and cooled ; it differs very little in appearance from plain zinc, out it is hard and duller, and contains 3 per cent, of iron and a little lead. See Percy's Metallurgy, Iron and Steel, p. 154. 1314. Alloy of iron and zinc produced experimentally. A hard compact mass, of grey tint and conchoidal fracture. 161 1315. Zinc containing 1 64 per cent, of iron. Shows a dull and irregular fracture. 1316. Alloy of zinc and iron. Fused with sulphur and cast into an ingot, like No. 1319. It shows the same spotted fracture. PRODUCTS OF THE PROCESS OF "GALVANISING" IRON WITH ZINC. 1317. Alloy of zinc and iron. This alloy has been produced in the process of galvanising iron. The result is a mass of small elongated rhombic crystals, similar to those of No. 1319. It contains 9-4 per cent, of iron. Communicated by T. H. Henry, Gospel Oak Works, Birmingham. See Percy's Metal- lurgy, Iron and Steel, p. 155. 1318. Spelter dross, from Ry lands' Galvanised Iron Works, Warrington. This is the ferriferous material that forms in the spelter bath, heated to a very high temperature in an open pot, then with a per- forated ladle the sediment is removed from the bottom of the pot, the holes allowing the liquid metal to pass through. This is an alloy of iron and zinc, and consists of minute examples of the same iridescent crystals as in No. 1282. Communicated by W. Dixon. 1319. Alloy of iron and zinc in an ingot. Produced in the process of galvanising as above. It is remelted and cast into these small square ingots, which are exported to India. Rylands' Galvanised Iron Works. The fracture is very irregular and platy, with numerous minute black spots. Communicated by F. Dixon. 1320. Alloy of zinc and iron. Produced in the galvanising process at the Arsenal, Woolwich, 1875. These are very well-formed rhombic prisms, with double pyramidal ends as in No. 1282. They are all of small size. Communicated by Mr. Charles. 1321. Alloy of zinc and iron, from Gospel Oak Works, Staffordshire. Obtained in galvanising iron. Contains about 5 per cent, of iron. This is in a solid mass, showing more needle-like crystals than the others, so far as it is separate. 1322. Zinc from among the bricks round a galvanising bath. One example shows a fine hair-like product, matted together, and having the general aspect of zinc, the rest are platy and brilliant. Communicated by F. Dixon, of the Galvanised Iron Company, War- rington. 1323. Residue from distilling ferriferous zinc lumps obtained in the process of galvanising iron. U 61955. 162 Rylands' GJ-alvanising Works, Warrington. An impure earthy- looking mass, probably consisting of iron oxide mixed with zinc and iron alloy. Communicated by F. Dixou. LEAD. THE PROPERTIES OF LEAD EXPERIMENTALLY ILLUSTRATED. 1324. Octahedral crystals of lead. Shown on the surface of glass which was being coated with lead in the process known as " quicking," by which the glass is made into a mirror. The glass is placed in a tray and heated to above the melting- point of lead, and melted lead is poured into the tray, and afterwards drained off. This specimen was produced by the lead accidentally being allowed to stay too long and to partially solidify. See Percy's Metal- lurgy, Lead, p. 1. Made by Mr. Matthews, of Birmingham. 1325. Lead wire, to show its feeble ductility. Communicated by P. Moore. 1326. Granulated lead, after exposure to the atmosphere. It has been entirely converted into sub-oxide, by the increase of its bulk by the absorption of oxygen. It burst the wooden box in which it had been contained. 1327. Litharge or protoxide of lead, which has been fused in a crucible. 1328. Litharge crystallised on metallic lead. This lead has been exposed to the joint action of air and water, which produced colourless transparent crystals of protoxide of lead, having the form of rhombic dodecahedra with truncated acute angles, and on heating in a tube they have become opaque and orange-coloured. See Yorke> Phil. Mag., 1834, p. 83; and Percy's Metallurgy, Lead, p. 14. Communicated by Colonel Yorke. 1329. Litharge passing into carbonate of lead. 1330. Litharge melted and coloured by cuprous oxide. A brownish black glass. 1331. Result of heating together copper sulphide with five times its weight of protoxide of lead. 400 grains of copper sulphide were mixed with 2,000 grains of litharge in covered crucible, and heated for about 10 minutes at a temperature just sufficient to effect perfect fusion. The result is a button resembling lead weighing 410 grains, and containing 5 -5 per cent, of copper, together with a slag of the two metallic oxides. Experiment by W. Baker. See Percy's Metallurgy, 1861, p. 261. 1332. Result of heating together equal parts of white lead and oxychloride of lead. It is a greenish-yellow crystalline mass. 163 1333. Result of heating together 750 parts by weight of litharge with 250 parts of oxychloride of lead. It is a brownish-yellow crystalline mass. 1334. Result of heating copper sulphide with 20 times its weight of protoxide of lead. JOO grains of copper sulphide were heated with 2,000 grains of litharge, and a button of metal was produced weighing 394 gains. It resembles lead, but contains 5 8 per cent, of copper. Experiment by W. Baker. See Percy's Metallurgy, 1861, p. 261. 1335. Result of heating 15 parts of litharge with one of red haematite. A liver-coloured crystalline mass. Experiment by J. F. Davis. 1336. Result of heating eight parts of litharge with one of red haematite. A darker-coloured solid mass, without obvious crystals. Experiment by J. F. Davis. 1337. Result of heating four parts of litharge with one of red haematite. A dark compact mass, except in the centre, in which are minute black crystals. 1338. Result of heating three parts of litharge with one of red haematite. A black mass with a crystal-lined cavity in the centre. 1339. Result of heating two parts of litharge with one of red haematite. A black semi-porous mass. 1340. Result of heating four equivalents of litharge with one of arsenious acid. 99 grains of arsenious acid were fused with 448 grains of litharge in a closed crucible. The product is compact homogeneous, wax-like, t)paque and pale orange colour, with a button of lead weighing 28 grains. Hence the arsenious acid has not been to any appreciable extent con- verted into arsenic acid. Experiment by R. Smith. See Percy's Metal- lurgy, Lead, p. 18. 1341. Result of heating together one equivalent each of litharge and white arsenic. 112 grains of litharge were fused at a dull red heat with 91 grains of white arsenic. The result is an opaque egg-yellow glass. 1342. Result of heating four equivalents of litharge with one of antimony. 194 grains of antimony in powder were fused with 672 grains of litharge in a covered crucible. The product is a brittle button of L 2 164 impure lead weighing 374 grains, and a glassy amber- coloured slag. Experiment by R. Smith. See Percy's Metallurgy, Lead. p. 19. 1343. Lead reduced by antimony. 500 grains of native antimony, 600 grains of sulphate of lead, 300 grains of nitre, and 300 grains of carbonate of soda were fused together. A button of lead was obtained weighing 70 grains, together with this crystalline slag of antimoniate of lead and soda, which has since decomposed on the surface. Experiment by R. Smith. 1344. Result of heating together three equivalents of oxide of lead and one of tin. 840 grains of lead oxide and 148 grains of granulated tin were taken. The result is not homogeneous, but contains some reduced lead. 1345. Result of heating two equivalents of litharge with one of iron. 140 grains of iron filings were fused at a bright red heat with 1,120 grains of litharge. The product is a button of lead weighing 530 grains, containing only a trace of iron, and a compact, semi-vitreous, dark brownish-black magnetic slag with shots of lead. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 21. 1346. Result of fusing three equivalents of litharge with one of silica. Melts at a comparatively low temperature, to an orange-coloured glass. Experiment by Dr. Beck. See Percy's Metallurgy, Lead, p. 29. 1347. Result of fusing two equivalents of litharge with one of silica. Melts easily to a bright yellow glass. Experiment by Dr. Beck. See Percy's Metallurgy, I.e. 1348. Result of fusing two equivalents of litharge with one of silica. In this case the product was allowed to cool slowly in the furnace. The result is a green-grey compact mass, with a coating of semi-trans- parent green glass on the surface. Experiment by Dr. Beck. See Percy's Metallurgy, I.e. 1349. Result of fusing three equivalents of litharge with two of silica. Melts easily to a dark orange-yellow glass. Experiment by Dr. Beck. See Percy's Metallurgy, I.e. 1350. Result of fusing one equivalent of litharge with one of silica. Melts easily to a light yellow glass. Experiment by Dr. Beck. See Percy, I.e. 165 1351. Result of fusing one equivalent of impure litharge with one of silica. In this case the litharge contained traces of iron and copper, and the result is a transparent green glass. Experiment by Dr. Beck. See Percy's Metallurgy, I.e. 1352. Result of fusing two equivalents of litharge with three of silica. This required a rather high temperature for its fusion, but the result is a yellow glass. Experiment by Dr. Beck. See Percy's Metallurgy, Lc. 1353. Result of heating one equivalent of litharge with two of silica. This required a high temperature for reaction, but fritted into a com- pact, whitej opaque, porcelain-like mass. This has been remelted at a still higher temperature, and poured out rapidly : a glass is thus with difficulty formed. Experiment by Dr. Beck. See Percy's Metal- lurgy, I.e. 1354. Result of heating one equiraleat of litharge with four of silica. At a very high temperature this was fritted into a compact porcelain- like, nearly white mass, very slightly porous. Experiment by Dr. Beck. See Percy's Metallurgy, I.e. 1355. Result of heating one equivalent of litharge with six of silica. This is an opaque porous mass, white with a greenish tinge. Experi- ment by Dr. Beck. See Percy's Metallurgy, I.e. 1356. Result of heating one equivalent of litharge with 12 of silica. This has been fritted in a white porous mass, scarcely cohering. Experiment by Dr. Beck. See Percy's Metallurgy, I.e. 1357. Silicate of lead from red lead and sand. Two equivalents of red lead were fused in platinum with one of silica. The result is a white powder. Experiment by R. Smith. 1358. Hollow globules obtained by heating silicate of lead with charcoal. The silicate is made by uniting one equivalent of litharge with one of silica ; it is intimately mixed with excess of charcoal powder, and strongly heated in a covered Cornish crucible. No button of lead is formed, but the result is a number of small hollow globules, of white or light yellowish-brown colour, opaque and vitreous, in fracture, and studded with small shots of lead. Experiment by Dr. Beck. See Percy's Metallurgy, Lead, p. 31. 1359. The same hollow globules mounted as microscopic objects. 166 1360. Silicate of lead containing one equivalent of lead oxide to one of silica. 5,000 grains of litharge wore fused with 2,034 grains of sand. The- result was a not very fluid green glass, which poured without difficulty at a very bright red heat. Experiment by Mr. Gribbs. 1361. The same silicate with some of the sand uncombined, 1362. Silicate of lead containing three equivalents of lead oxide to two of silica. 6,000 grains of litharge were fused with 1,628 grains of sand. This was more fluid than the last and poured more easily. It is a green glass, on account of the impurity of the litharge. Experiment by Mr. Gibbs. 1363. Silicate of lead containing two equivalents of lead oxide to one of silica. 5,000 grains of litharge were fused with 1,017 of sand. The result is a green glass, very fluid at a bright red heat. Experiment by Mr. Gibbs. 1364. The same silicate with purer litharge. In this case the glass is bright orange-coloured. 1365. Silicate of lead containing three equivalents of lead oxide to one of silica. 5,000 grains of litharge were fused with 678 grains of sand, and the product is a deep orange glass, very fluid at a bright red heat. Experi- ment by Mr. Gibbs. 1366. Results of experiments on the reduction of silicate of lead by iron. The silicate of lead, containing two equivalents of lead oxide to one of silica, was prepared by heating red lead with fine sand in a platinum vessel, at a temperature sufficient to frit but not to melt the mass. The temperature was afterwards raised to fuse it. When solid, the product was of an amber colour (a). It was poured, and 3,000 grains were heated in a wrought-iron crucible placed for protection against reduction in a clay crucible : at full redness lead began to separate, and the result was soft lead (>) ; 2,212 grains, and a black largely crystalline slag; (c) 1,418 grains: 1,115 grains of this slag were remelted in the same iron crucible for an hour, from which 13 grains of lead were obtained; and a crystalline slag (d) was left. This slag contains Protoxide of iron - 68-25 Sesquioxide of iron - 2-57 Protoxide of lead 82 Silica - 28-36 100-00 Experiment by K. Smith. See Percy's Metallurgy, Lead, pp. 34 and 533. 167 1367. Lead and galena fused together and cooled slowly. These were fused together in proportions of one equivalent each. The lead is found at the bottom of the mass, the galena at the top, but there is no very clear line between them. See Percy's Metallurgy, Lead, p. 39. 1368. Lead and galena fused together and cooled rapidly. The product is apparently homogeneous, intermediate in character between the two ingredients. See Percy's Metallurgy, Lead, p. 39. 1369. " Subsulphide of lead." In a dark coloured crystalline ingot. One half of the ingot has been heated to very low redness, without any lead sweating out of it. 1370. Result of heating sulphate of lead with lead. One equivalent of each yielded two equivalents of lead oxide. 760 grains of sulphate of lead were melted in an earthen crucible with 520 grains of finely granulated lead. The result is a small button of lead weighing 52 grains, and a dark amber-coloured glass, probably silicate of lead. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 46. 1371. Result of heating sulphate of lead with iron. 1,000 grains of the sulphate were heated to bright redness in a wrought-iron crucible, with the addition of iron nails. The result is a button of 520 grains of lead, out of the 681 grains contained in the sulphate. There is left 1,173 grains, dark coloured, imperfectly melted scoriaceous slag. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 45. 1372. Result of heating one equivalent of sulphate of lead with one of sulphide of lead. In this case the sulphur and oxygen in the ingredients are in the proper proportion to form sulphurous acid which is evolved, and a residue of metallic lead is left. See Percy's Metallurgy, Lead, p. 46. 1373. Result of heating three equivalents of sulphate of lead with one of sulphide of lead. In this case the sulphur can combine with only two thirds of the oxygen present, and protoxide of lead is left as a residue. See Percy's Metallurgy, Lead, p. 46. 1374. Result of heating one equivalent of sulphate of lead with two of carbon. The carbon forms carbonic dioxide with the oxygen, which is evolved, and the residue consists of sulphide of lead. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 51. 1375. Subsulphate of lead produced by fusing together one equivalent of lead sulphate with one of litharge. 760 grains of lead sulphate and 560 grains of litharge were taken. The result is a yellow sub-crystalline solid. Experiment by R. Smith. 168 1376. Result of heating one equivalent of sulphate of lead with one of carbon. Carbonic dioxide and sulphurous acid is given off and lead is left. 760 grains of sulphate of lead were fused with 30 grains of carbon, and the result is a button of lead weighing 105 grains, and a glassy amber- coloured slag probably silicate of lead, derived from the crucible. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 52. 1377. Result of heating one equivalent of sulphide of lead with two of protoxide of lead. In this case the sulphur and oxygen in, the ingredients are in the proportion to form sulphurous acid which is given off, and the residue left is lead. 560 grains of litharge were fused with 300 grains of galena, and there is a residue of 576 grains of metallic lead. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 45. 1378. Result of heating one equivalent of sulphide of lead with one of protoxide of lead. In this case the same reaction takes place, but half the sulphide is left unchanged in the midst of the reduced lead. 560 grains of litharge were fused with 600 grains of galena, and the resulting button weighed 962 grains. These resulting numbers both show great loss of lead. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 46. 1379. Result of heating sulphide of lead with haematite and carbon. 200 grains of hematite, 420 grains of galena, 35 grains of charcoal, were heated under 100 grains of salt. The result is a button of lead, covered by a dark glass, and this by an earthy slag. Experiment by R. Smith. 1380. Galena reduced by iron. The contents of the crucible after fusion are a button of lead at the bottom, and a metallic slag, covered with a glassy film. 1381. Impure sulphide of iron produced in assaying lead ores in an iron dish. See Percy's Metallurgy, Lead, p. 108. 1382. Result of heating together one equivalent of sulphide of lead with two of tin. The result is a button in two layers. The upper one vjery thin, crystalline, brittle, but yielding like talc, and friable. The lower one is easily cut with a knife, and shows a highly crystalline structure, with broad cleavage planes, and a blacker colour than galena, more like protosulphide of tin. Experiment by A. Dick, 1855. See Percy's Metallurgy, Lead, p. 59. 1383. Result of heating together one equivalent of sulphide of lead with two of tin. This is the same experiment as No. 1382, repeated on a larger scale, by R. Smith. 3,700 grains of galena were heated with 3,480 grains of tin, The result is very similar, showing the cleavnge planes of the 169 mass well. A small button of lead was also found at the bottom. Sec Percy's Metallurgy, Lead, p. 60. 1384. Result of heating together one equivalent of sulphide of lead with one of copper. These were heated in a covered crucible, and when fused consisted of two layers. The upper one is a brittle regulus, with a fine-grained bluish-grey fracture ; the lower one, soft malleable lead, containing 0-88 per cent, of copper. Experiment by R. Dick. See Percy's Metallurgy, Lead, p. 60. 1385. Result of heating together five equivalents of galena with one of zinc. The mixture was heated in a covered plumbago crucible, and covered with small pieces of charcoal. The product is crystalline, of deeper colour than galena. There was a small button of lead at the bottom. Experiment by R. Smith. See Percy's Metallurgy, Lead, p. 61. 1386. Result of heating sulphide of lead with antimony. The product is homogeneous, and powders before the knife; it is largely crystalline, and has a granular cleavage. There are air-holes, where it has been in contact with the crucible. The pieces of charcoal on the top are coated here and there with crystals of galena. This result shows that galena is not reduced when heated with antimony. Experiment by J. C. Cloud. See Percy's Metallurgy, Lead, p. 62. 1387. Result of experiment showing reduction of arsenite of lead. 650 grains of protoxide of lead, 495 grains of arsenious acid, and 60 grains of carbon, when heated together, produce a metallic button of lead, containing arsenic, weighing 380 grains, and capable of being beaten out. Experiment by R. Smith. The product of heating together the litharge and arsenious acid before adding the carbon is an opaque orange-yellow glass, as recorded by Percy's Metallurgy, Lead, p. 18. 1388. Result of heating together galena and phosphate of lead. 119-5 grains of galena and 182-5 grains of phosphate of lead were heated in a covered crucible, and left to cool slowly. The result is in two layers, the upper is of phosphate of lead, which is crystalline, and dirty green in colour, the lower of galena. There is, therefore, no reaction between these bodies at a high temperature. Experiment by J. C. Cloud. See Percy's Metallurgy, Lead, p. 76. ORES OF LEAD. 1389. Coarse crystallised galena from Devonshire. Contains 79 per cent, of lead and 4 oz. 15 dwt. 9 gr. of silver per ton. Communicated by Sir. L. Palk. 1390. Fine-grained galena from Devonshire. Contains 51 per cent, of lead and 2 oz. 5 dwt. 8 gr. of silver per ton. Communicated by Sir Lawrence Palk. 170 1391. Fine-grained galena from Cornwall. Communicated by Mr. Garby. 1392. Galena from Gogbam Lead Mines, near Aberystwith. Contains 30 oz. of silver per ton. 1393. Coarse galena from the New Red Sandstone, at Garendon, near Charnwood Forest. This is an accidental occurrence as an isolated mass ; not a vein. It is coarsely crystalline, and contains 81 per cent, of lead and 1 oz. 12 dwt. silver per ton. 1394. " Steel ore " from Snailbeach Mines, Shropshire. Communicated by Mr. Eddy. It is very fine-grained, compact pure galena, having somewhat of the lustre of fractured steel. 1395. " Blue stone " from North Wales. A complex ore, obtained at Pary's Mountain, Anglesea, containing sulphide of lead and sulphide of zinc, intimately mixed. See Percy's Metallurgy, Lead, p. 405. 1396. Coarse galena from Hornachos, Province of Badajoz, Spain. 1397. Coarse galena and blende intermixed, from Welkenradt, Belgium. Shows a concretionary structure in the gangue. I 1398. Galena from the Val-Sassam Mines. Contains 58 per cent, of lead and 49 oz. of silver per ton. 1399. Coarse galena from Arrayanez Mine, Linares, Province of Jaen, Spain. 1400. Granular galena from Ems, Nassau. 1401. Coarse galena, called " Potters' ore," or 2*84 \ Sulphuric acid 0-75 / Protoxide of lead - 36-87 Oxide of zinc 2-65 Lime- 1-63 Protoxide of iron - 0-90 Silica- - - - 1-10 99-78 See Percy's Metallurgy, Lead, p. 239. A loosely aggregated powder. 1456. Ore calcined for three hours in a reverberatory Flint- shire furnace. From Newton, Keats, and Co.'s Lead Works, Bagillt. Analysed by W. Weston. Sulphide of lead {^L I Us} 54 ' 56 Sulphate of 175 Protoxide of lead - - 27-18 Oxide of zinc 5-19 Lime - -1-96 Protoxide of iron - 1-33 Silica - - - - 1-85 99-74 See Percy's Metallurgy, Lead, p. 239. A loosely aggregated powder. 1457. Charge after setting up previous to pulverisation. Dee Bank Lead Works, 1859. 1458. Grey earthy slag from smelting galena. Dee Bank Lead Works, 1859. 1459. Grey slag from the ores of the district. Dee Bank Lead Works. A rough brown semi-scoriaceous mass. 1460. Skimming from the Flintshire furnace. This is taken from the surface of the lead towards the end of the smelting process. It has been remelted in a crucible. From Newton, Keats, and Co.'s Works, Bagillt. It is dark and sub crystalline. 1461. Black glassy slag for crushing and washing. This is " clean slag " from the blast furnace. It is crushed and washed to separate the intermixed spots of metallic lead. The remainder is thrown away. From the Bagillt Works. Analysed by W. Weston. Silica - Alumina Lime - Protoxide of lead Protoxide of iron Oxide of zinc - 99-40 See Percy's Metallurgy, Lead, p. 420. 1462. Skimming of furnace pot. From the Flintshire furnaces of the Dee Bank Lead Works. It is black, pulverulent, and crystalline. 1463. Grey slag from Cornish ores of high assay. This slag may contain from 40 to 50 per cent, of lead, and from 5 to 8 oz. silver per ton. From the Dee Bank Lead Works. A grey crystalline rough slab with large vertical holes. Communicated by A. B. Dick. 1464. Scum from the surface of the furnace pot. From the Flintshire furnace at Walker, Parker, and Co.'s. Containing most of the impurities of the lead. An irregular, heavy, scoriaceous black mass. Communicated by A. B. Dick. 176 1465. Slag from the slag hearth. From the Flintshire furnace at Alport, Derbyshire. Black and glassy, broken to small fragments. 1466. Run slag from the reverberatory furnace. From Alport Lead Works, Derbyshire. The composition of such a slag is given in Percy's Metallurgy, Lead, p. 241, but not of this sample. It is light coloured and strong, with tube-like holes. 1467. Drawn slag from the reverberatory furnace. From Alport Lead Works, Derbyshire. The composition of such a slag is given in Percy's Metallurgy, Lead, p. 241, but not of this sample. It is grey and stony. 1468. Run slag. From Llanelly Lead Works. A blue glassy slag, having the surface tinged with red. 1469. Black crystalline slag from the breast pan of the slag hearth. From the Lead Works at Alport, Derbyshire. 1470. Grey slag. A crystalline stony mass, weathering brown. From Newton, Keats, and Co.'s Works, Bagillt. 1471. Mean sample of grey slag. Ground to a powder. It may contain 50 or 55 per cent, of lead, and 1 or 2 oz. of silver per ton of lead. Walker, Parker, and Co.'s Lead Works. Experiments made at the Lead Smelting Works, Alston, to ascertain if scorification removes foreign metals or other im- purities from slag lead, 1848. 1472. Scoria from slag lead kept melted during four hours with access of air. It is now heavy and dark. 1473. Scoria from slag lead kept melted during eight hours with access of air. Nenthead Lead Works, Alston. It is now dark and cavernous. 1474. Scoria from slag lead kept melted during 12 hours with access of air. Nenthead Works. It is now light and irregular. 1475. Grey slag from smelting best ore. At the ore-hearth furnaces at Keld Head Mines, Wensleydale, York- shire. It is massive and earthy. Communicated by W. Weston. 1476. Slag from slag hearth in smelting inferior ore. Keld Head Works, Yorkshire. In small dull black fragments. 177 1477. Pounded white slag from ore hearth. The portion that passed through a sieve of 60 to the inch. Com- municated by W. Weston. 1478. White slag from ore hearth. The lead, &c. which is retained by the ^-inch sieve ; 452 grains out of 5,512 grains is thus retained. Communicated by W. Weston, 1479. Slags from smelting calcined Utah ores in a flowing furnace. From Dee Bank Lead Works, 1871. One is a black compact slag, glassy on the surface. The second is more slaggy, and the third, which is oxidised, is red in colour. 1480. Slag from smelting Australian sulphate ores. Produced at the Bagillt Smelting Works. See Percy's Metallurgy, Lead, p. 431. It is dull black and massive, with a few cavities. 1481. Matt from smelting Australian sulphate ores. From this the lead is obtained by two roastings and smeltings. See Percy's Metallurgy, I.e. Jt is a heavy sub-metallic dark slab. 1482. Slag from Australian lead ore. From the smelting of an earthy ore in a water-jacket furnace, 1886. It consists of brilliant black plates like those of silicate of iron. Com- municated by F. M. Drake. 1483. Slag from Australian lead ore. From a furnace in continual work where the object is the extraction of gold from pyrites with the use of as little lead as possible. It consists of brilliant interlocking acicular crystals. Communicated byF. M. Drake. 1484. Slag from Australian argentiferous lead ore. Smelced in a water-jacket furnace. It shows striated rhombic prisms like those of silicate of iron. Communicated by F. M. Drake. 1485. Lead slag with metallic lead found at Alston Moor. Supposed to have been produced in Roman lead works. 1486. Lead slag with pieces of charcoal imbedded in it, from Alston Moor. Supposed to have been produced in Roman lead works. It was found under cover of three feet of soil and turf near Bowgill Barn, a short distance from the Roman Road, in the Manor of Glassonby. 1487. Lead slag from old lead works at Loe Pool, Falmouth. It is compact and black, and slightly scoriaceous. 1488. Slags from lead smelting used in " sweep " smelting. The " sweeps " are the residues in gold and silver works, which are smelted with lead slags, &c. to recover the more precious metals. The history of these specimens is rather doubtful. U 61955. M 178 ACCIDENTAL PRODUCTS. 1489. Red lead formed in the bed of a reverberatory furnace, at the Dee Bank Lead Works, 1871. A crumbling cake. Communicated by A. B. Dick. 1490. Red lead formed in a smelting furnace. From the Alport Lead Works, Derbyshire. 1491. Lead and red lead found in an old reverberatory furnace at Pontesford, Shropshire. Found about 2 ft. 4 in. below the level of the surface of the working furnace bed, below the slags and below part of the brickwork. This furnace was not built on a double arch as is now done, and yielded when broken up and revived about 11 tons 3 cwts. 3 qrs. of refined lead. Communicated by Mr. Eddy. 1492. Silvery micaceous litharge. Found in taking up the bed of a calciner at the LlanellyLead Works, 1859. Communicated by Mr. Williams. 1493. Deposit which forms in the flues of the litharge furnaces. At Benson's White Lead Works, Birmingham. It is stalactitic in form, red inside, and grey and crumbling outside. 1494. Yellow micaceous litharge. From the bed of the lead calcining furnace at Nenthead, Alston. 1495. Crystallised sulphide of lead. Formed in the bed of a reverberatory furnace at the Dee Bank Lead Works, 1871. It is now disintegrated. Communicated by A. B. Dick. 1496. Crystallised product from the smelting furnace at Dee Bank Lead Works. The crystals in the cavity are micaceous and may be litharge. 1497. Concretions under the test of a cupellation furnace. From Gossage's White Lead Works, Birmingham, 1841. They are long complex stalactitic masses of decayed lead. 1498. Microscpic slide of crystalline litharge. From the base of a calciner at the Llanelly Lead Works, South Wales. 1499. Artificially crystallised sulphide of lead. Brilliant hopper-shaped crystals, forming an incrustation from a lead smelting furnace, at Regla, near Real del Monte, 1846. Communicated by Mr. Broomhead, of Birmingham. 1500. Artificially crystallised sulphide of lead. A furnace product from the Wahsatch Smelting Works, U.S.A. Some of this shows a purple lamina due to the intermixed metallic impurities. 179 The crystals are not well formed, but appear to be cubic. Communicated by Mr. Blackwell. 1501. Concretion from the protoxide furnace. Formed in the production of lead in the dry way, by oxidising the ore in a reverberatory furnace. From Messrs. Atkins' Works. PATTINSON'S PROCESS FOR THE EXTRACTION OF SILVER FROM LEAD. 1502. Specimens of hard lead from slag smelting. Nos. 1, 2, and 3, of different hardness, previous to submission to Pattinson's process. Communicated by H. L. Pattinson, 1849. 1503. The original lead put into the fourth pot. It contains 9 oz. 16 dwt. silver per ton of 21 cwt. 1504. The first crop of crystals obtained from the fourth pot. These contain 4 oz. 4 dwt. 16 gr. silver per ton of 21 cwt. 1505. The second crop of crystals obtained from the fifth pot. These contain 2 oz. 7 dwt. silver per ton of 21 cwt. 1506. The third crop of crystals obtained from the sixth pot. These contain 1 oz. 3 dwt. 12 gr. silver per ton of 21 cwt. 1507. The fourth crop of crystals obtained from the seventh pot. These contain 10 dwt. 23 gr. silver per ton of 21 cwt. 1508. The melted lead from the market pot. Called " horn lead," being the melting of the crystals obtained from the seventh pot, and containing only 10 dwt. 23 gr. silver per ton of 21 cwt. PARKES' PROCESS OF DESILVERISATION. 1509. Piece of Belgian retort, after use in smelting the lead. 1510. Argentiferous zinc crust, taken off the molten lead. From the Llanelly Lead Works, 1859. This contains most of the silver in the lead, viz., 275 oz. 8 dwt. per ton. See Percy's Metallurgy. Lead, p. 152. 1511. First skimming of the molten lead, after taking off the crust. From the Llanelly Lead Works, 1859. M 2 180 1512. Lead liquated out of the zinc crust. This contains 55 oz. of silver per ton, but should not contain more than 10 oz. See Percy's Metallurgy, Lead, p. 152. 1513. Portion of the zinc crust, after the lead has been liquated out of it. 1514. Zinc distilled from the liquated zinc, and cast in the form of a bar. 1515. The silver powder left as a residue, after the zinc has been distilled off. An earthy grey powder containing the silver. 1516. Slag from the run-down silver powder. It is massive, compact, and cavernous. These are all (Nos. 1509-16) from the same process as carried on at the Llanelly Works in 1859. 1517. Zinc alloy taken from the lead in Parkes' process. This has been subsequently liquated to withdraw a portion of the lead. It now has the composition Silver - - - - - 3*13 Lead - 73 '42 Copper - 2-07 Arsenic - 3*49 Antimony - - - 0*19 Zinc - - - - 16-84 Iron - trace Insoluble residue - 25 99-39 Analysed and communicated by J. G. Hochstatter, at Par Smelting Works, Cornwall, 1870. In small earthy lumps. 1518. Lead rich in silver after distilling off the zinc. This is a further stage of the same process. From the Par Smelting Works, 1870. Communicated by J. G. Hochstatter. 1519. Zinc containing silver from the skimmings of the zinc alloy. From the Par Smelting Works. In a fine powder called "scum powder." 1520. Dross from the softening furnace. This is produced in the treatment of the lead contaminated with zinc. It contains the impurities after the lead has been softened by Parkes' process. From the Llanelly Lead Works, 1859. See Percy's Metal- lurgy, Lead. It is heavy, scoriaceous, and earthy-looking. 1521. Ingot of desilvered lead now ready for the softening furnace in Parkes' process. From the Llanelly Lead Works, 1859. 181 1522. Ingot of lead after softening. This has had the impurities partially removed (see No. 1518) by heating in the softening furnace, and is now ready for the poling pot. From the Llanelly Lead Works, 1859. 1523. Desilvered softened lead after poling. This is the softened lead tapped off from the softening furnace into a cast-iron receiver, where it is " boiled " or poled by submerged wood, and is now ready for the market. From the Llanelly Lead Works, 1859. CORDURI'S PROCESS. 1524. Oxide from near the charging door of the silver blast furnace in Cordurie's process. This is produced in the dezincification of lead by steam, passed through the molten mass, whereby the impurities and part of the lead are oxidised, and blow away as powder. It contains 17-85 per cent, of lead, and 37 oz. 11 dwt. of silver to the ton. From the Par Smelting Works, 1870. Communicated by J. Gr. Hochstatter. 1525. Powdery deposit in the chimney, in Cordurie's process of steaming lead. This contains 6-22 per cent, of oxide of lead. From the Par Smelting Works. Communicated by J. G. Hochstatter. 1526. Another powdery deposit in the chimney, in Cordurie's process of steaming lead. From the Par Smelting Works. Communicated by J. G. Hochstatter. PURIFICATION OF HARD LEAD. 1527. Sample of " hard lead." Contains antimony, arsenic, copper, nickel, cobalt, and possibly other ingredients. It shows a brilliant crystalline surface on one side, with platy and octahedral crystals. 1528. Slag lead from Atkins' Works, Derbyshire. This is a hard lead, and requires to be softened. It has soft, rounded, radiating fibres. 1529. Crystals from hard lead, from very coarse ore. They are dull and platy. 1530. Substance obtained in the liquating of hard lead. At the Dee Bank Lead Works, Bagillt. The upper lamellar portion is a speiss ; the lower is in soft small pyritic crystals. Communicated by A. Dick. 1531. Speiss obtained from the lead smelted in a flowing furnace. Contains much antimony, and probably some cobalt. A layer of regulus is seen on the top. 182 1532. Result of smelting hard lead, with various residual substances, containing lead, mixed with a poor coppery regulus,. to separate copper from the hard lead. This mass of hard lead, containing silver, when molten, was left to- cool slowly. It consists of three parts. The top part contains Lead - - 42-22 Iron - 19-39 Copper - 11-15 Antimony - 4 . 93 Sulphur - - - - 21-41 99-10 This is, therefore, a regulus. The middle part is crystalline, granular, and like pig-iron in structure, and of the colour of antimony. The lower, largely crystalline, and foliated part, contains Lead- - 57-83 Tin - 9-40 Copper 2-44 Iron - 0-18 Nickel - - - 0-89 Antimony - - 27-55 Arsenic 0-62 Sulphur 0-52 99-43 Analysis by W. J. Ward. See Percy's Metallurgy, Lead, p. 467,. and Silver and Gold, p. 669. 1533. Results of experiments on liquating hard lead. (1.) Liquated lead : granulated. (2.) Residual lead, last poured out : dull and soft. (3.) Sulphide after liquation : grey dust with pyritous lumps. (4.) Sulphide that first comes to the surface on melting : broadly crystalline and dull. 1534. Lead liquated from copper, first stage. 1535. Lead liquated from copper, second stage. LEAD FUMES. 1536. Lead fume from the flue of the smelting furnace. From the Bagillt Lead Works, 1859. This sample is made from portions of fume taken at different distances out of the main flue, into which the short flues enter, from 10 yards, at intervals of 50 yards. Analysed by W. Weston. Protoxide of lead - 46-54 Sulphide of lead 4-87 Iron oxide and Alumina 4-18 Zinc oxide - 1-60 Lime - 6-07 Sulphuric acid - 26-51 Insoluble - 10-21 99-98 See Percy's Metallurgy, Lead, p. 451. A reddish-white powder. 183 1537. Lead fume deposited at the bottom of the stack. From the Bagillt Lead Works, 1859. This consists of the mixed fumes of the smelting furnaces and slag-hearth. Analysed by W. Weston. Protoxide of lead - - -62-26 Sulphide of lead 1 05 Iron oxide and Alumina 3-00 Zinc oxide - - 1-60 Lime - 3-77 Sulphuric acid - 25-78 Insoluble - - - 1-97 99-43 See Percy's Metallurgy, Lead, p. 481. A white powder. 1538. Lead fame from the slag-hearth. From the Bagillt Lead Works, 1859. Taken from the slag-hearth flue before its junction with the main flue. Analysed by W. Weston. Protoxide of lead - 46-88 Iron oxide and Alumina - 10-00 Zinc oxide - - - 4-14 Lime- 6-73 Sulphuric acid - 14 '15 Insoluble - 14-40 Carbonaceous matter from fuel 3-37 99-67 See Percy's Metallurgy, Lead, p. 451. A grey powder. 1539. Lead fume as taken from the condenser. From the Keld Head Lead Works, Wensleydale, Yorkshire. A dark grey aggregated powder. 1540. Series of lead fumes from different parts of the same condensing system. Probably from the Keld Head Lead Works, Yorkshire. Nos. 1, 2, 3, 4 position not stated. No. 5 from above the little condenser. No. 6 from the top of the chimney. No. 7 from the cistern. No. 8 position not stated. They are light coloured powders of various shades, the darkest being No. 6. 1541. Four samples of lead fumes from the Alport Lead Works, Derbyshire. No. 1 is from the first condensing chamber in connexion with the slag-hearth, and is an aggregated grey dust. Nos. 2-4 are from the return flue, after passing through the condenser. No. 2 is lighter grey. No. 3 nearly white. No. 4 light brown. 1542. Another series of lead fumes from the Alport Lead Works, Derbyshire. Locality in' flue not stated. They nre labelled Nos. 2, 3, 4. No. 2 is the darkest ; the others are light brown, or nearly white. 184 1543. Fume from the cupelling hearth. From a German lead works. It is called " Frisch Raust," and is a hite powder. ILLUSTRATIONS OF SMELTING COMPLEX ORES, CONTAINING LEAD AND OTHER METALS, AS CARRIED ON IN THE HARZ. PRIMARY OPERATIONS. 1544. Compact galena. The lead ore on which the operations are made. 1545. Once-roasted lead ore, " 1-mal gerostetes Bleierz." It is now brown and lighter. 1546. Twice-roasted lead ore, " 2-mal gerostetes Bleierz." A dark brown earthy mass. 1547. Thrice-roasted lead ore, " 3-mal gerostetes Bleierz." In small brown earthy fragments. In the preliminary process of roasting the ore, sulphur is given off, which is recovered as below 1548. Raw sulphur from the roasting, " Rohschwef el." Cast into a thin cake. The thrice-roasted ore is smelted with zinc slag. 1549. Calamine or silicate of zinc from whence the zinc is obtained, " Galmei." An impregnated slate. 1550. Zinc reduced in the process. Covered with a coat of slag. 1551. Slag, " Schlacke." A hard regulus-like mass, with large cavities. The products obtained are 1552. Blast-furnace lead, " WerkbleL" The basis of the refining operations. For analysis, see Percy's Metallurgy, Lead, p. 312. 1553. Furnace accretion, " Ofenbruch." Consisting of a mass of minutely crystallised stalactitic impure lead. 1554. Marl-bottom of the furnace, " Lehmsohle." This becomes impregnated with the litharge, and also more or less melted. 1555. Lead regulus, " Bleistein." This contains a portion of the lead which has afterwards to be worked. Tt is a massive slabby substance, and contains the impurities including copper. For analysis, see Percy's Metallurgy, Lead, p. 313. 185 The next operations are performed upon the blast-furnace lead (No. 1552), refining it by means of cupellation, yielding the following products 1556. Scum, " Abzug." This is the rubbish which forms on the surface of the lead when molten, and consists of a mixture of dark earthy fragments, containing oxide of lead with the impurities which may be present. 1557. Skimming poor in lead, " Bleiarmer Abstrich." A stony decaying mass, consisting mostly of litharge, being formed after the removal of the Abzug ; it is sometimes called " black litharge." See Percy's Metallurgy, Lead, pp. 194, 201. 1558. Skimming rich in lead, " Bleireicher Abstrich." An earthy-looking mass, consisting of a purer mixture of litharge with other materials, taken off at a later stage of the cupellation. 1559. Litharge for reduction, " Frisch-Glatte." This is the last product to be driven off and collected in a molten form. It is now white, earthy, and crumbling. 1560. Brightened silver, " Blicksilber." This is the mass that is left after the lead has been oxidised and driven off. When the mass loses the last trace of litharge it suddenly brightens, and is then Blicksilber. This contains numerous large rounded cavities below the surface, formed by the gas which did not escape, and which raises the surface into hills. The whole mass is composed of finely arborescent silver crystals. The upper surface has a thin layer of yellow vitreous oxide of lead. It has been analysed bv R. Smith, and contains 96-95 per cent, of silver. See Percy's Metallurgy, Lead, p. 196. 1561. Marketable litharge, " Kauf-Glatte." Consisting of red and white scales of tolerable purity. 1562. Furnace bottom, " Heerd." Marl strongly impregnated with litharge. See Percy's Metallurgy, Lead, p. 203. The working up of the Scum, " Abzug." On smelting this the following three substances are produced 1563. Lead for operations, " Werkblei." A sample of the impure lead. 1564. Regulus from the scum, " Abzugstein." A porous irregular stony mass, containing much metal. 1565. Slag, " Schlacke." A blue glassy mass, with large holes. 186 The lead thus obtained is now liquated, and produces 1566. The more purified lead for operations, " Abzugswerk- blei." A sample from the lead liquated from the copper and other impurities, except silver. 1567. Liquation rubbish from the scum, " Abzugsaigerkratz." A mass of mixed materials including charcoal. The first of these products is now cupelled as the first lead was, and yields 1568. The scum, " Abzug." This includes all the rubbish that collects on the surface of the molten lead, in separate small pieces. 1569. First skimming, " Abstrich." A dark impure litharge material. 1570. Second skimming, (( Abstrich." A solid mass of greenish impure litharge. 1571. Litharge, " Glatte." Flowing off at a later stage as a micaceous mass. 1572. The residual Blicksilber from this process, to obtain which is its object. A swollen doubly convex mass, with a cavity inside and a tail-like process. 1573. Furnace button, ; ' Heerd." Marl, richly impregnated with litharge, and which will be worked up again with it when the litharge is reduced. The liquation rubbish is also smelted, and produces a mass of workable lead, some slag, and 1574. Regulus from the liquation rubbish, " Abzugsaigerkratz- stein." A porous crumbling mass, which contains all the copper. On smelting and treating this in a suitable manner, there are obtained 1575. Refinery slag, " Verblasenschlacke." A reddish stony mass, which forms the bulk ; and 1576. The refined copper, " Gaarkupfer." In the form of a long hollow finger. 1577. Roasted lead regulus, " Gerostete Bleistein." This is the result of the first operation. It is then smelted, and yields three products. A dark loose cinder. 187 1578. Poor lead from liquating, " Armwerke. This consists of the lead which has been liquated off, and which con- tains all the silver there was in the copper, but this does not amount to- very much. The treatment of the Lead Regulus. 1579. Slag, Schlacke." A blue-tinted compact regulus-like mass, with large flat holes and a blistered surface. 1580. Furnace regulus, " Rohstein." A crystalline |-inch slab, the subject of future operations. 1581. Black copper, " Schwarzkupfer." This is dark and granular in fracture, and requires much refining,, but the operation is not connected with lead. The furnace regulus is again roasted, forming roasted regulus, " Rohrost," not in the collection, and afterwards smelted, pro- ducing 1582. Dark regulus from the roasted regulus, " Rohroststein." A thin sub-metallic blistery substance which is again operated on y yielding a second crop of copper. 1583. Black copper, " Schwarzkupfer." Of arborescent crystalline form, to be still further treated for ob- taining copper. 1584. Slag, Schlacke." A light sub-metallic-looking thin sheet with large holes. The black copper when refined yields granulated copper, " Granalien," and refinery slag, '' Verblasenschlacke," but these are not in the collection. The dark regulus is again roasted, and yields 1585. Roasted regulus, " Gerostete Rohroststein " or " Kupfer- rest." An irregular cinder-like dark mass. This is afterwards smelted, and yields a third crop of copper. 1586. Black copper, " Schwarzkupfer." A porous mass, forming the final product so far as the lead processes are concerned. 1587. Thin matt, " Stein." A very thin metallic-looking covering with vertical holes, used again in combination with other products. 1588. Slag, " Schlacke." A hard, solid, metallic-looking crust, also worked up again. 188 1589. Lead regulus, " Bleistein." A porous earthy mass. The result of smelting the ores in the blast furnace, Freiberg. 1590. Roasted lead regulus, " Gerostete Bleistein." A cindery brown mass ; the first result of the second operation. 1591. Lead slag, Bleischlacke." A compact dark mass with large holes, glassy below, and with flow lines and fragments above. 1592. Regulus slag, " Bleisteinschlacke." The slag produced in the first operation, a rough mass full of holes, and with fragments of unsmelted ore. 1593. Litharge refinery slag, " Glattfrischeschlacke.' The slag produced in the later refining process ; a very scoriaceous dark mass. LEAD WORKING AT MULDNER HUTTE, &c.. FREIBERG. The series from Freiberg (so labelled) is very incomplete. 1594. Lead regulus, " Bleistein," from Halsbruckner Hiitte. This is the result of previous operations on mixed ores containing both copper and lead. A 1^-inch compact slab with cavities. 1595. Lead regulus, "Bleistein," and speiss from Muldner Hutte. This is a porous, dark, heavy mass with mixed metallic contents, and having a thin coating of speiss containing arsenic and antimony. 1596. Lead speiss, Muldner Hiitte. The antimonious lead regulus obtained in smelting. It is a IJ-inch metallic, broadly crystalline slab. 1597. The lead obtained from the lead regulus, " Bleistein- werke." This has to be afterwards subjected to refining processes, and is, there- fore, called " Werke." 1598. Speiss from Bleistein smelting, Muldner Hiitte. Another more massive example of the antimonious regulus, with irregular crystals of a golden colour. 1599. Lead slag, " Bleischlacke." From the lead workings at Muldner Hiitte, but the stage is not stated. It is apparently in part metalliferous. A solid, black, sub- metallic slate. 1600. Lead obtained from the smelting of coarsely powdered galena, " Schliegwerkblei." 189 The ore is first ground to coarse powder called " Schlieg," before being smelted : this is the first product of the reduction by iron, it has afterwards to be refined. See Percy's Metallurgy, Lead, p. 369. 1601. The first skimmings of the already scorified molten lead, " Abstrich." This is the first coating of impurities after the scum, or " Abzug," in the cupellation furnace. Consists of a mixture of litharge and other materials in compact masses. 1602. The second skimmings of the molten lead, " Abstrich." The litharge in this is a more abundant ingredient, and it is more crystalline aud regular, forming a. thin slab. 1603. Litharge ready for reduction, " Frisch-Glatte." A yellow, micaceous, crumbling mass, consisting of the pure litharge after the . See Percy's Metallurgy, Silver and Gold, p. 87. 1771. A mixture of silver sulphide, copper chloride, and com- mon salt exposed in solution to the air for five years. The mixture is now a green liquid and with a white precipitate. 1772. Compound ? produced by the action of silver on mercuric chloride, in proportions to form silver chloride and mercurous chloride. 1773. Sulphide of silver derived from silver chloride. In the form of a black powder. By acting on the chloride dissolved in sulphate*of soda by hydrochloric acid. 1774. Action of sulphide of lead on chloride of silver. A mixture of these two compounds, in proportion of one equivalent of each, was fused in a hard glass tube at a dull red heat. The fused mass consisted of two layers : the upper one, almost entirely soluble in water, was mostly chloride of lead ; the lower layer is black, dense and sectile, soluble in nitric acid, and is mostly sulphide of silver, containing 72 '53 per cent, of silver out of the 87-1 per cent, it would contain if it were pure. Experiment by U. Louis. See Percy's Metallurgy, Silver and Gold, p. 101. 1775. Bromide of silver formed by acting on silver leaf by the vapour of bromine. Grey metallic fragments, retaining the form of the leaf. 1776. Result of heating together silver and phosphorus. To 501 grains of molten silver in a clay crucible, 200 grains of red phosphorus were added in successive portions with stirring. After the surface had become smooth, the metallic mass on cooling rose in the crucible to nearly double its volume, giving out phosphorus vapour. It is vesicular in the upper part and solid underneath. The metal in the upper part is rather yellowish white and crystalline, in the lower part it is clearer white and more solid. The upper part was found to contain 0-293 per cent, of phosphorus, and to contain 0-072 per cent, of phos- phorus in addition in the form of phosphoric acid in the cavities. The lower part contained 0-207 per cent, of phosphorus. Experiment by R. Smith. See Percy's Metallurgy, Silver and Gold, p. 137. 1777. Silver compound analogous to the purple of Cassius. If hydrated peroxide of tin is stirred into a thin milky liquid, a neutral solution of nitrate of silver added, and the mixture gently heated, this substance, purplish-brown when dried, is produced, con- sisting of stannate of tin and stannic hydrate, or possibly of the latter 207 only and metallic silver. Experiment by H. Louis. See Percy's Metallurgy, Silver and Gold, p. 128. 1778. Arsenide of silver. 501 grains of silver were melted under charcoal in a clay crucible, and 201 grains of metallic arsenic added in three successive portions. The metallic mass was well stirred till the surface was tranquil and then allowed to cool. The product is hard and brittle, its fracture is granular and slightly crystalline, dark iron-grey, and dull in lustre, but becoming bright by burnishing. It contains silver 8] '46 per cent, and arsenic 18 '54 per cent., and corresponds therefore approximately to the formula Ag 3 As. Experiment by R. Smith. See Percy's Metallurgy, Silver and Gold, p. 139. 1779. Compound of three equivalents of silver and one of antimony. 162 grains of silver were melted under charcoal in a clay crucible, and 61 grains of antimony added by degrees. The metal was well stirred, and taken out of the furnace to cool. The product weighed 222 8 grains, showing a loss of two grains. It is harder than silver, its fracture is largely crystalline, and its colour is bluish white. Ex- periment by R. Smith. See Percy's Metallurgy, Silver and Gold, p. 143. 1780. Compound of four equivalents of silver and one of antimony. 216 grains of silver and 61 grains of antimony were operated upon in a similar manner to the last. The product weighed 276 grains, show- ing a loss of one grain. The colour is greyish white, but otherwise the product resembles the last. Experiment by R. Smith. See Percy's Metallurgy, I.e. 1781. Compound of six equivalents of silver to one of antimony. 162 grains of silver and 30-5 grains of antimony were similarly acted on. The product weighed 192 grains, showing loss of -5 grain. Its fracture is granular and the colour greyish white. Experiment by R. Smith. See Percy's Metallurgy, I.e. 1782. Result of heating together oxide of silver and oxide of antimony in atmospheric air. A mixture of equal bulks of the two oxides was heated to low redness in a glass tube open at both ends, and slightly inclined so that a current of air kept passing through it. The product is a dull greenish-grey mass, which gives reduced silver when heated in a closed tube ; 19-165 grains of this on analysis gave 5 '31 5 grains of chloride of silver and 10-713 grains of antimony, corresponding to 22-44 per cent, oxide of silver and 75 87 per cent, antimonic acid. Experiment by H. Louis. See Percy's Metallurgy, Silver and Gold, p. 146. 1783. Antimoniate of silver heated. A greenish-grey powder. 208 1784. Alloy of silver and antimony in the proportion of one equivalent each. 42 per cent, of silver and 58 per cent, of antimony were heated together, producing a dark grey brittle mass. Experiment by G. H. Hochstatter. See Percy's Metallurgy, Silver and Gold, p. 147. 1785. Calcined alloy of silver and antimony. The alloy produced in the last experiment was finely powdered and heated, with free access of air. The product, is brownish yellow, and contains metallic silver. On analysis it contains Oxide of silver - - 34 Metallic silver - - - 37-20 Antimonious acid - - -62-89 100-43 Experiment by G. H. Hochstatter. See Percy's Metallurgy, I.e. 1786. Alloy of silver and antimony calcined with ferrous sulphate. A mixture of 50 grains of the finely powdered alloy (prepared as in No. 1784) and 20 grains of dry ferrous sulphate was calcined in air. The product is a dark brown powder, containing metallic silver. Its analysis gives Metallic silver - - 30-92 Ferric oxide - - - 15-23 Antimonious acid - 53-90 100-05 1787. Metal produced in an attempt to prepare silicide of silver. Contains 92-04 per cent, of silver, 4-90 per cent, of lead, 0-15 per cent of aluminium, and 2-77 per cent, of uncombined silicon. Experi- ment by L. Jackson, 1875. SILVER ORES. 1788. Silver ore from Avrastras, Real del Monte. 1789. Silver ore for amalgamation. Contains 171 oz. 3 dwt. 21 gr. to the ton. 1790. Pyrargyrite, ground, a sulphide of silver and antimony. 1791. Proustite, ground, a sulphide of silver and arsenic from MarienLerg. 1792. Silver ore from Valparaiso. Containing 30 per cent, of silver in the form of ground chloride ; also some arsenic. 209 1793. Fused chloride of silver from Africa. Probably from sand containing it. Communicated by Rose, Norton, and Co. 1794. Silver-lead ore from Spanish Mine, Bingham Canon, Utah. A soft grey stone. 1795. Silver-lead ore from Davenport Mine, Little Cottonwood District, Utah. A dark heavy sub-metallic mass. 1796. Silver-lead ore from Miner's Delight Mine, East Canon, Ophir Mining District, Utah. Grey and scoriaceous. 1797. Silver ore from MoHeriry's Mine, Parley's Park Canon, Utah. Grey and sub-metallic. Communicated by the Utah Mining Company. 1798. Mass of brown quartz sh owing ciystals of native silver. New South Wales. 1799. Silver-lead ore from San Juan Mine, Mexico. Analysed by R. Smith. Contains 63 per cent, of lead and 44 oz. 3 dwt. 17 gr. silver to the ton of ore. Communicated by Stevenson Forbes, Llandudno. 1800. Silver ore from Morning Star Mine, Butte, Montana. In a gnngue of pyritous quartz. In 1881 this mine had produced 600 tons of ore, containing 135 oz. silver and 1 oz. gold to the ton. Communicated by W. A. Clarke. 1801. Ore containing zinc, copper, and iron. Butte, Montana. Dark and sub-metallic, yields 160 oz. silver to the ton. Communi- cated by W. A. Clarke. 1802. Silver ore from Mintton Mine, Butte, Montana. Massive and speckled. Produce $45 worth of silver per ton, 1803. Silver ore. Lexington Mine, Butte, Montana. An earthy gossan. Communicated by W. A. Clarke. 1804. Ruby silver ore from Sheridan Mine, San Miguel County, Colorado, U.S.A. In a massive quartzose gangue. 1805. Silver ore from Mexico. Earthy brown ore containing sulphide of silver, in the rough state ; some is ground to powder for the purposes of amalgamation. U 61955. 210 1806. Silver chloride ore, or horn silver. From "Big Pittsburg Mine," Leadville, Colorado, U.S.A. ; very rich in chloride of silver. Heavy, brown, and earthy. Communicated by Dr. Johnson. 1807. Silver ore from Little Sliver Mine, Leadville. Colorado, U.S.A. Brown and ochreous. Contains chloride of silver. 1808. Silver ore from Kobert E. Lee Mine, Leadville. Colorado, U.S.A. Red and ochreous. Contains chloride of silver. 1809. Bismuth -silver ore from the Geneva district, Colorado. A dark grey brecciated vein. THE SMELTING OF SILVER GEES. SERIES of SPECIMENS showing the Method of Silver-working at the Morfa Silver Works, South Wales. Supplied by the late Richard Pearce when Manager, 1869. 1810. Mixed silver ore ground to powder. This contains about 400 ounces of silver to the ton. It is smelted with the two succeeding specimens. 1811. Crushed slag metal. This consists of dark fragments derived from the silver-ore slag after smelting it with mundic. It forms part of the mixture for the primary smelting. 1812. Gossan, Surface- weathered product, used to form part of the mixture for the primary smelting of the ores. 1813. Silver metal regulus. 20 cwts. of mixed silver ore, 10 cwts. of crushed slag metal, and 5 cwts. of gossan are smelted together, and the products are this black porous regulus, containing about 2 5 per cent, of silver and 10 per cent, of copper, and the following slag. 1814. Silver-ore slag. Accompanying the regulus No. 1813. A black glass taken from the top of the slag where rapid cooling occurs. 1815. Silver-ore slag. Accompanying the regulus No. 1813. Taken from the middle of the slag. It contains, on an average, about 10 ounces of silver to the ton. Massive, black, and vacuous. 211 1816. Mundic to smelt with the silver-ore slag. The products are the slag metal used in the primary smelting, and the next substance. 1817. Slag from smelting silver-ore slag (Nos. 1814, 1815) with mundic (No. 1816). A massive, black, compact slag, said to be clean, i.e., not to contain any metal worth extracting. The final product of the smelting process is No. 1813; this is then treated by Ziervogel's process for the extraction of the silver as sulphate. 1818. Silver-metal regulus, ground and passed through a sieve of 60 holes to the linear inch. 1819. Ground silver-metal regulus calcined for eight hours. The silver which is present in the form of sulphide is thus converted into a soluble sulphate, while the copper, iron sulphides, &c. with which it is contaminated become sulphates sooner, and are now converted into insoluble oxides. 1820. Residue after washing No. 1819 with hot water for about 12 hours. The sulphate of silver is by this washing extracted in a soluble form, and this residue contains about * 20 per cent, only of silver (= 65 oz. to the ton) and 10 per cent, of copper. 1821. Silver in flakes as precipitated from the solution of the sulphate by plates of copper. 1822. Silver precipitate after washing with dilute sulphuric acid. This washing separates the copper and copper oxide, and the residue, a clear silver-white powder, is fit for melting, and should contain 99*80 per cent, of silver. The larger amounts of silver having thus been extracted, further processes are resorted to for the extraction of the residue, and the metal contained in poorer ores ; the following 15 specimens (Nos. 1823 to 1837) illustrate this process. They are all communicated by Mr. E. Pearce, of the Morfa Silver Works, South Wales. 1823. Mixture of argentiferous ores, raw and calcined. This contains about 5 per cent, of copper and 4 to 5 oz. of silver to the ton. This is mixed with " sharp " slag (see No. 1829) in the pro- portion of 30 cwt. of the former to 5 cwt. of the latter. 1824. Ore metal from smelting No. 1823. It is solid, sub-metallic, with a brownish lustre, and is full of cavities ; it contains about 38 per cent, of copper and 30 oz. of silver to the ton. 1825. Slag accompanying the ore metal, No. 1824. It is a crystalline black slag with small cavities, and is thrown away as worthless. o 2 212 1826. Ore metal (1824) crushed and calcined during 30 hours. 1827. White metal. This is obtained by smelting No. 1826 with siliceous argentiferous ore rich in^ copper, or " cobbing " (old bricks, &c.). It is black, heavy, and glistening, and usually contains about 70 per cent, of copper and 80 oz. of silver to the ton, in the form of sulphides. 1828. Sharp slag, A solid mass without grain or obvious crystallisation, except at the surface, which is covered with a loose aggregation of arborescent crystals, in the form of minute octahedra of magnetite (?), with a few. brown transparent plates of iron-silicate. 1829. Sharp slag. This is the other product which accompanies No. 1827. It is blue black, brilliantly metallic, with crystals in the cavities, and is used for the primary smelting in this process. See No. 1823. The white metal is then subjected to ZiervogeFs process for the extraction of the silver as sulphate. 1830. White metal crushed previous to calcination. 1831. Crushed white metal after calcination for 24 hours, 1832. Calcined white metal, ground and passed through ,** sieve with 80 holes to the linear inch. 1833. The ground calcined white metal recalcined for the production of sulphate of silver. This has been calcined four additional hours, whereby the silver sulphides become sulphates, and the already produced copper sulphates become oxides. 1834. Residue after washing out the sulphate of silver. It usually contains about 24 oz. of silver to the ton,, which has not been converted into sulphate by the process. The sulphate is treated with copper plates as before. This residue is then subjected to Augustin's process for the extraction of the silver as chloride. 1835. Product of the calcination of JS [ o. 1834 with salt for the production of chloride of silver. 1836. Residue after washing No. 1835 with strong hot solution of salt. This salt solution removes the silver chloride, and this residue contains about 6 oz. silver to the ton, 1837. Silver precipitated as a grey powder from chloride solution by copper plates. It is afterwards boiled with hydrochloric acid, to separate copper and lead. This is the final product of the process, and is melted with the silver obtained by precipitation in the Ziervogel process. 213 1838. Blister copper obtained by melting the residue (No. 1836) with coal. It is sent to the copper works. For the whole process thus illus- trated, see J. A. Phillips' Mining and Metallurgy of Silver and Gold, p. 409, &c. 1839. Four varieties of regains obtained by smelting various South American silver ores at Liverpool. They contain a great variety of metals, and are not further dealt with in the works where they are smelted. They are all reduced ta powder. 1840. Argentiferous regulus for the Ziervogel and Augustin processes. Two specimens from Morfa Silver Works, 18fi9, really duplicates of No, 1827* but of rather different aspect. One is massive, with brilliant platy crystals ; the other compact dark brown, with cavities. 1841. Matt from smelting mixed silver ore. No locality given. A speiss-like 1-inch slab with irregular cavities. 1842. Slag from smelting silver ore in the flowing furnace. Ground to a coarse black powder. 1843. Slag from Grant Smelting Company, Leadville. Very solid, and with a brown lustre. 1844. Kegulus from smelting silver ores. It is speiss-like, with irregular cavities, in a 1^-inch slab. It consists of sulphides and arsenides of iron, &c. 1845. Slag from smelting argentiferous residues from zinc pots. The zinc is derived from blende, and iron pyrites is used to collect the silver. Two specimens of dull opaque, semi-vitreous substance^ with a scoriaceous surface. 1846. Argentiferous and auriferous copper matt. A solid, crystalline, sub-metallic mass, called (i white metal," ready for " stripping." Black Ha*,vk, Colorado. 1847. Argentiferous copper matt. A thick copper slab, scoriaceous in parts, called "purple metal," After stripping the white metal. Black Hawk, Colorado. 1848. Gold and silver regulus slag. Produced in the process of smelting " sweeps " from gold and silver- smiths' shops. At Betts' Refinery, Birmingham, 1845. It consists of a compact matt below, and a coating of reddish-black glass above. 1849. Lead slag used in gold and silver sweep refining at Betts' Refinery, Birmingham. 214 It contains a certain amount of lead, and this extracts the gold and silver from the " sweep " on smelting. It is grey, earthy, and scori- aceous, with crystals in the cavities, and is probably from Derbyshire. See No. 1488. 1850. Slag from " sweep " refinery. From Bett's Works, Birmingham. Contains numerous black acicular crystals. These appear to be the crystals measured by Professor Miller, and described by Dr. Percy in the Eeport for 1846 to the British Association on Crystalline Slags. They belong to the oblique system, and are not identified with any known mineral. AMALGAMATION PROCESSES. 1851. Roasted ore ready for amalgamation. Freiberg. A brown powder. 1852. Silver amalgam squeezed. Contains one-sixth part of silver, and is now ready for retorting. Comstock Mines. Communicated by R. J. Frechville. 1853. Crude bullion, or retorted amalgam. From " Crown Point Mine," Comstock Lode, Nevada, U.S.A. A rough button, containing about 94 per cent, of silver and 4 per cent, of gold. Communicated by R. J. Frechville. 1854. Silver obtained as a solid button by heating the solid amalgam. Mexican amalgamation method. 1855. Arborescent silver, " Ausglich silber." Solid below, with parallel black stalactites. From the Halsbruckner Amalgamation Works, Freiberg. REFINING SILVER BY CUPELLATION. 1856. " Vegetable silver." This has " spit " into a remarkable rose-like form. In the process of refining silver by mixing it with lead, and then cupelling, the silver, as it becomes refined, absorbs a large quantity of oxygen, and towards the end of the process this oxygen is given out again like steam from water, and throws the silver into fantastic shapes. From the Black Hawk Silver Works, Colorado, 1875. For an account of this form of silver, see Percy's Metallurgy, Silver and Gold, p. 14. Communi- cated by R. Pearce. 1857. Refined silver, in an irregular cup-like form, of a brilliant metallic white. This has spit in a similar manner. In the accompanying tube is shown the trace of gold obtained from 102-13 grains of this silver. 1858. Two cupel buttons of silver. 215 ABNORMAL PRODUCTS IN SILVER WORKS. 1859. Slag containing reduced silver in hollow cavities. No history is attached to this; it is dark, earthy, porous, and brown. 1860. Silver-ore slag, containing arsenious acid and metallic arsenic. A black cinder-like mass, with crystalline arsenic in small cavities. From the Morfa Silver Works, 1869. See No. 1835. Communicated by R. Pearce. 1861. Silver-ore slag, containing metallic arsenic in cavities on the surface, This slag was formed from smelting silver ores, containing a large quantity of arsenic ; it was tapped from the furnace, and allowed to remain in the bed for 36 hours. It is accompanied by small selected crystals of arsenic. Morfa Silver Works, 1866. Communicated by R. Pearce. 1862. Argentiferous and auriferous copper matt, " Coarse metal." From Boston and Colorado Works, Black Hawk, Colorado. Compact, brown, sub-metallic, with fine holes. This and the eight following (Nos. 1863-1870) were all communicated by R. Pearce, 1875.. 1863. Furnace bottom product containing free gold visible in the cracks of the compact rock. Black Hawk, Colorado. (Three specimens.) 1864. Furnace bottom product containing metallic, brilliant white plates and octahedra in a thin sheet. Black Hawk, Colorado. 1865. Furnace bottom product with purple - tarnished octahedral crystals in small cavities. Black Hawk, Colorado. 1866. Argentiferous copper matt with the surface showing octahedral crystals. Black Hawk, Colorado. 1867. Argentiferous and auriferous copper matt with the surface showing arborescent crystals, arranged in skeleton octahedra. Boston and Colorado Works, Black Hawk, Colorado. 1868. Crystals from a silver-smelting furnace bottom. They came from immediately above the brickwork of the arch forming the vault of the furnace, below the furnace bottom proper, and from a part that had not been disturbed for five or six years. The crystals are partly dark octahedra, resembling bornite, and partly 216 brilliant white platy crystals, a rough analysis of which gives silver 40 per cent., lead 40 per cent., and gold 3 per cent. Black Hawk, Colorado. 1869. Artificial galena. From a furnace bottom, smelting silver ores at Black Hawk, Colorado. The furnace bottom is composed of pieces of gneiss, in the interstices between which the galena is also found. 1870. Artificial galena with white crystals on the surface. From Black Hawk, Colorado. Compare No. 1868. The galena crystallises perpendicular to the surface of a dark stony mass. 1871. Crystals resembling olivemte from a furnace bottom. They are from a metal furnace bottom which had been working five years, and are formed on some bricks immediately resting on the arcli supporting the bottom. Two specimens showing a bluish incrustation of small crystals. From the Morfa Silver Works, Swansea, 1870. This and the following eleven (1872-1882) were all communicated by B. Pearce. 1872. Artificial copper pyrites from a furnace bottom. The massive dark yellow crystalline substance has the appearance, specific gravity, and composition of copper pyrites. It is from an ore furnace which had been in work four years, and occurred sparingly in some vertical joints and fissures. Morfa Silver Works, 1870. 1873. Substance resembling copper pyrites from a furnace bottom. Morfa Silver Works, 1870. It is a cracked mass of matt, the surface of the cracks and of some stalactitic droppings are coloured a metallic yellow, but this appears to be superficial. 1874. Furnace bottom product. Morfa Silver Works, 1870. A calcined lump showing green radiating crystals of some copper salt. 1875. Substance resembling iron pyrites from a furnace bottom. Morfa Silver Works, 1870. Compact and massive, of a rather dull brownish-yellow colour, 1876. Crystallised sharp slag. The surface mainly consists of brilliant flat plates overlapping each other, and arranged so as to form a hollow box with prismatic edges. Here and there on the surface are clusters of dull octahedra. It thus resembles the crystalline forms of the silicates of iron formed in iron furnaces. From Morfa Silver Works, 1870. 1877. Crystallised sharp slag. The whole of the surface is covered with needle-like outgrowths, each of which is composed of a large number of superposed octahedral 217 crystals, possibly of magnetite, but having a peculiar tarnish. From Morfa Silver Works, 1870. 1878. Speiss from an old furnace bottom at Morfa Silver Works. The long prismatic crystals resembling stibnite have a specific gravity of 7 308, and have been analysed by Mr. Holdich at the Morfa Works, and yield Arsenic - - 43*75 Antimony - 20-95 Copper - 12-50 Iron - - 12-85 Nickel and Cobalt - 4-90 Bismuth, Lead, and Silver - 3-00 Sulphur - 2-30 100-25 1879. Another example of a similar speiss. In this case the brilliant prismatic crystals are interspersed with and overgrown up some dull tinted arborescent crystals. Morfa Silver Works, 1870. 1880. Black scale-like crystals on the surface of a furnace- brick. It is suggested that these crystals are oxide of copper pseudomorphous after chloride of copper. They occurred on the surface of and impregnating old bricks which formed part of a salting calciner at the Morfa Silver Works, 1869. 1881. Crystals of cupreous oxide formed on the surface of the copper plates used to precipitate silver from its sulphate solution. They are scales off the plates, with a minutely crystalline surface. From the Morfa Silver Works, 1869. 1882. Piece of one of the wooden precipitation vats at Morfa Silver Works, after incineration, 1871. The silver is precipitated in the fibres of the wood, and this is after- wards incinerated, and a large quantity of silver recovered. The specimen is therefore a model in silver of all the vessels and cavities in the substance of the wood. 1883. Furnace product from a silver reduction works at Salt Lake City, United States. Communicated by E. S. Black well, 1874. Brilliant crystalline plates standing erect, and composed of numerous smaller hexagonal and rectangular plates. They are a mixture of lead, copper, zinc, and silver- 218 1884. Crystals believed to be disulphide of copper. From one of the furnace bottoms at the Boston and Colorado Silver Smelting Works, Denver, 1880. 1885. Crystals of red oxide of copper artificially produced. These minute crystals were found in clusters attached to the sides of a wooden cistern, which was used for the recovery of the last traces of silver from the solution of the sulphate in Ziervogel's process. They are one year's growth, the cistern being annually cleaned, the tempera- ture being pretty constant from 180 to 200 Fahr. Boston Silver Smelting Works, Denver, 1880. 1886. Artificially crystallised copper. Minute pieces coated with grey dust obtained from one of the bottoms of the furnaces used for roasting white metal for the concentration of the gold. Boston Silver Smelting Works, 1880. 1887. Two specimens of a brilliant crystalline furnace bottom alloy. Produced in the smelting furnaces of the Boston and Colorado Smelting Company, Colorado, 1883. It consists of outgrowths, of octahe- dra and octahedral plates, sometimes in spear-like forms, sometimes in rectangular or oblique arborescent form. Roughly analysed, it consists of gold 19-88 per cent., silver 39-07 per cent., and lead 41-05 per cent. 1888. Brick from calcining furnace showing absorption of silver. This was taken from the bottom of a calcining furnace which was employed for some weeks in oxidising a granulated alloy containing 84 per cent, of copper and 16 per cent, of silver. The heat used was at no time above a good cherry-red heat, sufficient to completely oxidise the copper. The brick contains 4 2 per cent, of silver, and 3 6 per cent, of copper. Communicated by J. F. Williams. From Llanelly Lead Works, J883. 1889. Clay between the bricks of a calcining furnace showing absorption of silver. This is the intervening material between the bricks, No. 1888. In this case the clay has absorbed 8-5 per cent, of silver and 3-6 per cent. of copper. These specimens point to the conclusion that the silver is ex- tracted in the form of aluminate or silicate by the porous clay and brick, but little copper being taken with it, and that the unburnt clay has a stronger action in this respect than the brick. Llanelly Lead Works, 1883. Communicated by J. F. Williams. THE METAL IN VARIOUS FORMS. 1890. " White Pine" silver bullion cast into an ingot. From the White Pine Mine, Comstock Lode, Nevada, U.S.A. Con- tains 99*5 per cent, of silver, weight 12-83 oz. Communicated by E. J. Frecheville. 219 1891. Silver precipitated from the sulphate in irregular pieces. 1892. Silver specially purified. In a precipitated granular form, prepared by A. Dick. 1893. Silver purified by cupellation, in a solid button. 1894. Silver showing columnar fracture. Melted silver was poured at the Morfa Silver Works into an open mould of the usual shape,' and fractured by a blow of a hammer. Near the upper edge of the fracture, in the neighbourhood of the point of percussion, the metal consisted of a confused aggregate of imperfectly formed octahedral crystals (upper specimen), elsewhere it is fibrous and columnar, the fibres nearly perpendicular to the sides and bottom of the ingot (lower specimen). See Percy's Metallurgy, Silver and Gold, p. 3. 1895. Purified silver in the form of a button containing 99 ' 76 per cent, silver and 1 per cent. gold. 1896. Figure in " Pina silver " from Mexico. Weight, o ounces 264 grains, 1879. 1897. Pure silver wire. 1898. Silver leaf. Showing the tarnishing it suffers on exposure. ALLOYS OF SILVER.* 1899. Alloy of 95 parts of silver to 5 of aluminium. 1900. Alloy of silver and zinc, containing * 18 per cent, of silver. 600 grains of zinc were heated to as near the melting point of the metal as possible, and 12 grains of silver added. After half an hour the silver on cooling was found in its original solid state at the bottom, hence at this temperature very little solution of silver takes place. Experiment by G. H. Godfrey, 1870. See Percy's Metallurgy, Silver and Gold, p. 169. 1901. Alloy of silver and zinc, containing 8 16 per cent, of silver. Produced by heating 600 grains of granulated zinc and 60 grains of granulated silver to strong redness under charcoal for half an hour. It has a specific gravity 7-44. It is bluish grey, hard, brittle, easily scratched with a knife, and with a granular fracture. Experiment by G. H. Godfrey. See Percy's Metallurgy, Silver and Gold, p. 170. * Exclusive of those with arsenic and antimony. 220 1902. Alloy of silver and zinc, containing 22 47 per cent, of silver. Produced by pouring molten zinc into molten silver, when violent action ensued. It has a specific gravity 7 -62 is bluish grey, harder than No. 1901? brittle, less easily scratched, with a bright fibro-colnm- uar fracture. Experiment by G. H. Godfrey. See Percy's Metallurgy, I.e. 1903. Alloy of silver and zinc, containing 49 72 per cent, of silver. Produced in the same way as No. 1902. It has a specific gravity 8-61, and is copper-red on the surface and fracture when hot, but white and bright when cold. It is very hard and brittle, the fracture is foliated or columnar, inclining to conchoidal. Experiment by G. H. Godfrey. Sec Percy's Metallurgy, Lc. 1904. Alloy of silver and zinc, containing 67 "58 per cent, of silver. Produced in the same way as No. 1902. It has a specific gravity 9-30. It has a faint yellowish tinge, and is hard and brittle. Its fracture is columnar, and its colour is white at first, but tarnishing to yellow. Experiment by G. H. Godfrey. See Percy's Metallurgy, I.e. 1905. Alloy of equal parts of silver and thallium. Made by Mr. Crookes, 1876. The two metals readily fuse together ; tha alloy is somewhat, but not completely malleable. They are easily separated on a cupel, the thallium very rapidly oxidising, as on this specimen ; when the surface is freshly scraped, the colour is white. See Percy's Metallurgy, Silver and Gold, p. 17.5. 1906. Semi-liquid amalgam of silver and mercury. Obtained in experimenting on South American ores. 1907. Solid amalgam of silver and mercury. 1908. Alloy of two parts of silver and one of platinum. Used by dentists for artificial palates, and also as a standard of electrical resistance, &c. Prepared in sheet by Johnson, Matthey, and Co. See Percy's Metallurgy, Silver and Gold, p. 182. 1909. Alloy of silver [and platinum ?]. Annealed, and unannealod, after rolling into a sheet, like the last. 1910. Alloy of three parts of silver and one of palladium. Rolled out into a very thin sheet. It does not blacken by sulphuretted hydrogen, but these specimens are much tarnished. See Percy's Metallurgy, Silver and Gold, p. 182. 1911. Silver containing gold and iridium. In a small thin sheet from Messrs. Betts' Refinery Works, Birming- ham. Silver is said to form no alloy with iridium alone. See Percy's Metallurgy, Silver and Gold, p. 183. 221 1912. Filings of an alloy of silver and tin. Used to form an amalgam with a small quantity of mercury for stopping teeth, sold as Smale's Dental Compound. It is said to contain 60 per cent, of silver and 40 per cent, of tin. 1913. Alloy of silver with 20 per cent, of magnesium. Prepared by J. Parkinson in rock salt and fluor-spar. It has a yellowish tint, and cracks on being beaten out. See Percy's Metallurgy, Silver and Gold, p. 188. 1914. Alloy of silver containing 10 per cent, of magnesium. In a small yellow tarnished button. See Percy's Metallurgy, I.e. 1915. Alloy of silver and cadmium. Used for graduated scales of philosophical instruments. Analysed bv R. Smith. Silver - - 86 '66 Copper ' 02 Cadmium 13 '34 Gold - 0-02 100-04 See Percy's Metallurgy, Silver and Gold, p. 668. 1916. Alloy of silver and gold in a plate, such as is used for parting. Made by Johnson, Matthey, and Co. 1917. Alloy of 49 parts of silver to 51 of copper. Yields by cupellation 48 '3 of silver. Made by R. Smith, and beaten- into a sheet. 1918. Alloy of 89 parts of silver to 11 of gold. Made by R. Smith, and beaten into a sheet. 1919. Alloy of 32 parts of silver with 51 parts of copp00 grains of hard ore were heated with 250 grains of anthracite in^a^der, 125 grains of lime, 190 grains of clay, and 260 grains of sancfr The resulting metal is white iron, and contains 85 per cent, of silicon. The reduction is not complete. [The description on the label and in the " Metallurgy " do not entirely agree.] 2622. Result of Experiment VIII. 1,000 grains of the hard ore were heated with 200 grains of anthra- cite, 125 grains of lime, 190 grains of clay, and 260 grains of sand ; and the mixture was covered by a thin layer of anthracite powder. The resulting metal contains 0-38 per cent, of silicon, and the accompanying green slag has the per-centage composition of lime 19, alumina .11-55, silica 69-45. 2623. Result of Experiment IX. 1,000 grains of hard ore were heated with 250 grains of anthracite, 125 grains of lime, 190 grains of clay, 1,400 grains of sand ; 50 addi- tional grains of anthracite powder were placed on the top of the mixture. The resulting iron weighed 387 grains, and contains 1 15 per cent, of silicon. The accompanying slag is green. 2624. Result of an unrecorded experiment. 1,000 grains of the hard ore were heated with 250 grains of anthra- cite, 190 grains of clay, and 350 grains of lime. No proper button is formed, but a white stony slag, with scattered globules of metal. 2625. Result of another unrecorded experiment. 1,000 grains of the hard ore were heated with 250 grains of anthra- cite, 190 grains of clay, and '325 grains of lime. The result is a white scoriaceous stony slag, with numerous metallic globules. 2626. Wrought iron melted in 15 minutes from a T 5 F square bar in a closed clay crucible/ 2627. Attempt at the union of ferric oxide with alumina, A mixture in the ratio of the equivalents was strongly heafed in a platinum crucible. The result is a slightly coherent mass, without evidence of union. Experiment by E. Smith, 1871. The same mass reheated in a clay crucible has produced a black glassy substance. 2628. Attempt at the union of ferric oxide and lime. A mixture in the ratio of the equivalents was strongly heated in a platinum crucible contained within a crucible of lime. A portion has run together into a black slag. The remainder is still in powder. Experiment by R. Smith, 1871. 297 2629. Attempt at the union of ferric oxide and lime. A mixture in the ratio of the equivalents has been strongly heated, but only a certain amount of adhesion is brought about. Experiment by E. Smith, 1871. 2630. Micaceous oxide of iron produced artificially. By heating crystals of sulphate of iron with salt, and washing the precipitate with water. 2631. Production of slag by the union of haematite and limestone. 160 grains of ferric oxide have been heated with 100 grains of carbonate of lime, and the product is a dark, opaque, slag -like mass. 2632. Result of experiment with a soft ore. This ore contains only 6 36 per cent, of matter insoluble in hydro- chloric acid, of which 1 87 per cent, is silica. This has been heated with excess of charcoal, and has yielded a metal containing 1 66 per cent, of silicon. 2633. Result of another experiment with the same ore. It was fused with fine sand, and an excess of charcoal, and the metal produced contains 5-15 per cent, of silicon. 2634. Results of experiments on the production of silicides of iron. By E. Riley. Dowlais Iron Works, 1871. A mixture of red hema- tite ore, with charcoal in excess, and siliceous sand, from crushed washed sandstone, was made and fused after exposure in a plumbago steel-pot in a Siemens 1 furnace for 36 hours. The fused mass of iron at the bottom (No. 1) was about 3 Ibs. in weight. It contains 17-96 per cent, of silicon. Much of the sand retained its granular form, with fused cinder (No. 4) between the granules containing scattered buttons of iron (No. 3), which contain 3-72 per cent, of silicon. There are also many buttons suspended in the charcoal (No. 2), which contain 21-71 per cent, of silicon. 2635. Results of another experiment of the same kind. In this case silicate of iron was first formed from the same red ore as above, by mixing it with sand and a little charcoal, after pulverising it, and mixing the whole with wood charcoal, and exposing it in a plum- bago pot in a Siemens' furnace for 36 hours. Siliceous cinder (No. 6) was perfectly fused, and the mass of iron at the bottom (No. 5), which was about 4 Ibs. in weight, is highly crystalline in fracture, with large graphitic scales, and contains 17 40 per cent, of silicon. Communi- cated by E. Riley. 2636. Result of experiment on the union of silicide of iron with phosphide of iron. 220 grains of silicide of iron, containing 8-96 per cent, of silicon, were mixed with 143 grains of phosphide of iron, containing 12-66 per cent, of phosphorus. The mixture was heated in a covered clay crucible placed within another, and heated during 1 hour to whiteness 298 The button produced weighed 356 grains, and had a little slag on the top. It is hard, brittle, and strongly magnetic. Its fracture is crystal- line, but dull, and its colour light greyish-white. It contains 5-57 per cent, of silicon, and 4-50 per cent, of phosphorus. Experiment by Mr. Hochstatter. See Percy's Metallurgy, Iron and Steel, p. 95. 2637. " Silicate of protoxide of iron." Prepared by W. B. Richardson. The proportions employed were haematite 47'1, silica 57-5, and anthracite 6 per cent. This mixture was heated to whiteness in an iron crucible. It is highly vesicular, dark olive brown in colour, opaque, brittle, and vitreous. It contains 33 per cent, of iron. See Percy's Metallurgy, Iron and Steel, p. 96. 2638. " Trisilieate of protoxide of iron." Prepared by W. B. Richardson. 2,400 grains of iuematite, 900 grains of pure white sand, and 180 grains of powdered anthracite being in the proportions of 78-1, 29-8, and 6 per cent, were treated in the same way as in the last experiment. The product weighed 3,070 grains, showing 70 grains to have been derived from the iron crucible. It has a bright almost metallic lustre, is brittle and crystalline, the cavities con- taining crystals of iron olivine. It contains 54 per cent, of iron. See Percy's Metallurgy, Iron and Steel, p. 96. Results of a series of experiments on the carburisation of iron by cementation. Nos, 2639-2644. See Percy's Metallurgy, Iron and Steel, p. 105. 2639. Strips of iron prepared for experiments by means of hydrogen. 2640. Result of Experiment 4. The strip of iron was imbedded in sugar charcoal and heated in a porcelain tube during two hours in a current of hydrogen, and allowed to cool in the gas. The charcoal had already been used in a similar experiment. The strip increased in weight from 15-385 to 15-550 grains. 2641. Result of Experiments 5 and 6. The curved pieces were treated by imbedding one in the previously used charcoal and not the other, and passing hydrogen over them at a red heat. The free strip increased in weight from 5-405 grains to 5-425 grains. The imbedded strip increased from 5-805 grains to 5 -850 grains. The free strip is more dead in lustre and the other is deeper grey. The unbent portions were treated in a similar way. 2642. Result of Experiment 9. 2643. Result of Experiment 10. The strips were placed in two long glass tubes. In one the strip was imbedded in the same charcoal as used in previous experiments, and both were heated in hydrogen for three and a half hours. The free strip has increased in weight from 9-458 grains to 9-468 grains. The im- bedded strip increased from 10-081 grains to 10-133 grains. 299 2644. Result of Experiment 11. The last experiment was repeated with two free strips and electrotype iron, the hydrogen having been passed through nitrate of silver and over pumice wetted with sulphuric acid. The free strips have increased from 9-086 grains to 9-150 grains; the imbedded one from 5-026 grains to 5-080 grains. 2645. Experiment on the absorption of carbon by pure iron. Conducted by R. Dick. Ferric oxide obtained .from iron wire was intensely heated with excess of carbon. The result is a number of but- tons and globules. The buttons have a specific gravity of 7 097. They split when hammered, and show plates of graphitic carbon, amounting in various trials to three or four per cent. See Percy's Metallurgy, Iron and Steel, p. 113. 2646. Another experiment on the same subject. The ferric oxide was obtained from ferrous sulphate. The result is a multitude of small globules which will not fuse together on reheating. The largest button has a different fracture, a specific gravity of 6 968, and contains graphite to 4 56 per cent. See Percy's Metallurgy, Iron and Steel, p. 114. 2647. Mixture of grey and white cast iron. The crystals of the white iron form a rectangular complex network, belonging to the cubical system, the sheets in a horizontal direction being the most conspicuous, with the grey iron in the interstices between them. Compare Percy's Metallurgy, Iron and Steel, p. 116. 2648. Experiment on the combination of iron with carbon. Tin plate iron has been heated with chemically pure charcoal. The result is a very graphitic iron containing 4^ per cent, of carbon. 2649. Results of Messrs. Baker and Stuart's experiments on the conversion of soft iron into steel by means of carbonic oxide. (a.) Specimen of a very soft iron used in the experiment. It is manufactured by Messrs. Marshall and Mills, Wednesbury. One of the pieces is straight, the other has been heated to a full red heat and quenched as in hardening steel ; nevertheless, it remains perfectly soft and has been bent cold. (6.) Part of the same iron converted into steel by the action of carbonic oxide passed over at a full red heat for 12 hours. The carbonic oxide was prepared from oxalic acid and sul- phuric ncid. The evolved gas was passed through milk of lime, caustic potash, and pyrogallic acid, and dried by sulphuric acid, (c.) Another portion of the same steel broken in pieces to show its brittle- ness. The transverse section shows a central core of unconverted crystalline soft iron, surrounded by the fine grained steel, showing the depth to which the conversion has penetrated. Experiments conducted in 1864. Communicated by Win. Baker. Compare Percy's Metallurgy, Iron and Steel, p. 105. 300 2650. Spiegeleisen melted under plate glass. This does not show any separation of graphite or any sensible change in the external characters of the metal'. See Percy's Metallurgy, Iron and Steel, p. 121. Results of experiments on the action of sulphur on iron con- taining carbon conducted by W. Weston, recorded in Percy's Metallurgy, Iron and Steel, pp. 135, 136. Nos. 2651-2654. 2651. Result of Experiment 7. 376 grains of cast iron were melted with 64' 5 grains of iron sulphide, which is equivalent to introducing 4 378 per cent, of sulphur. The product is white iron, without graphite. It contains 2 '12 per cent, of sulphur, showing a loss of 2 '258 per cent. The carbon is 3 '17 per cent. 2652. Result of Experiment 8. 359 grains of cast iron were melted with 29 grains of iron sulphide, which is equivalent to introducing 2 '235 per cent, of sulphur, for half an hour. The button consists of very crystalline white iron, with separated graphite. The metal contains 1 68 per cent, of sulphur. .The carbon amounts to 3 '9 per cent., of which 1*44 per cent, is graphitic, the remainder being in combination. 2653. Result of Experiment 9. 415 grains of cast iron were melted with 18 grains of iron sulphide, which is equivalent to introducing I '243 per cent, of sulphur. The product is white iron, with separated graphite. The analysis showed 1'313 per cent, .of sulphur (which must be in error). The carbon amounts to 3 6 per cent. 2654. Result of Experiment 10. 302 grains of cast iron were melted with 7 '2 of iron sulphide, which is equivalent to introducing 0*696 per cent, of sulphur. Some graphite separated. The metal is not white, but grey, with a network of white iron. The analysis showed 0'72 per cent, of sulphur (which must be in error). 2655. Result of experiment on heating grey pig-iron with sulphide of iron. 8,800 grains of grey pig-iron were melted in a clay crucible under plate glass with 870 grains of sulphide of iron containing 29 '9 per cent, of sulphur. The metal here obtained has the appearance of white iron. It is brittle and excessively hard. The centre is more or less hollow, and shows a few skeleton crystals. The fracture is uneven and rather lamellar. It contains 0*78 per cent, of sulphur. Experiment by R. Smith, 1858. See Percy's Metallurgy, Iron and Steel, p. 133. . 2656. Result of the action of sulphur on gtey iron. 1,540 grains of grey pig-iron were melted with 90 grains of iron sul- phide,-equivalent to 2 per cent. The product is a hard white iron, with a 301 somewhat lamellar fracture. It contains 0' 78 percent, of sulphur, Compare Percy's Metallurgy, Iron and Steel, p. 133. 2657. Grey pig-iron remelted. 2658. Result of experiment on the action of manganese containing carbon on iron containing silicon. A very white metal is produced. 2659. Result of experiment on the heating of spiegeleisen containing manganese with feme oxide. 2660. Formation of silicate of iron by the action of copper. Six equivalents of copper, one of ferric oxide, and two of silica, were heated with abundance of charcoal, hsematite being employed which contained the above proportion of silica. A union of the silica and iron has taken place. Experiment by R. Smith. 2661. The slag which accompanied the silicate of iron in the above experiment. 2662. Result of heating together 400 grains of roasted Wicklow pyrites, 15 grains of carbon, and 150 grains of silica. The result is a pyritous button accompanied by an opaque blue glassy slag. Experiment by R. Smith. 2663. Result of an experiment on Wicklow pyrites. 3,500 grains of roasted ore, 131 grains of charcoal, 1,312 grains of silica, and 960 grains of cast iron have been smelted together. The products are (a) a light porous black shining slag, together with a minute particle of gold derived therefrom ; (b) the button of iron left at the bottom ; (c) a button obtained after treating part of the iron with lead ; (d) minute particle of gold derived from the iron. 2664. Result of another experiment in heating grey pig- iron with sulphide of iron. 10,600 grains of another variety of grey pig-iron were melted during about an hour in a clay crucible, under plate glass, with 327 grains of sulphide of iron, containing 29 ' 9 per cent, of sulphur. The metal produced contains 0*91 per cent, of sulphur, showing a loss of 0*815 per cent. The surface is coated with dark glass. A cut surface shows a mottled network of bright crystalline meshes. Experiment by R. Smith, 1858. See Percy's Metallurgy, Iron and Steel, p. 134, exp. 4. ALLOYS OF IKON. 2665. Experiment on the fusion of spiegeleisen and copper. 500 grains of each have been fused together, showing a loss of 3*4 per cent. The product consists of copper below and spiegeleisen above, but the copper contains 1 18 per cent, of manganese and 3 * 19 per cent, of iron. Experiment by J. Richardson. 302 2666. Another experiment on the same subject. 666*45 parts of iron have been melted with 334 parts of copper. The loss on fusion has been 2 '35 per cent., and the copper surrounds the iron with a dark intermediate layer between. Experiment by J. Richardson. 2667. Alloy of 10 of copper with 2 of iron. 200 grains of iron wire with 1,000 grains of electrotype copper were fused under plate glass, in a clay crucible, with luted cover. The result is a well melted button, showing a loss of 8 grains. It is much harder than copper, but the fracture is copper-red in colour. It has a granular fracture, but cannot be drawn into wire. Experiment by J. Richardson. See Percy's Metallurgy, Iron and Steel, p. 149. 2668. Alloy of 10 of coppc-r with 3 of iron. 300 grains of iron and 1,COO grains of copper were heated together at a red heat. 55 grains of iron remained unfused, and the button has a paler colour, but is not so tough. It appears to be homogeneous, and contains 20 per cent, of copper. Experiment by J. Richardson. See Percy's Metallurgy, Iron and Steel, p. 149. 2669. Alloy of 5 of copper with 7 of iron. 500 grains of copper and 700 grains of iron were melted together as before. The button is well melted with a loss of 6 grains. The surface of the alloy is grey, liko iron, and appears to be coated with it; it, is crystalline and brittle, having minute crystal faces. It contains 58^ per cent, of iron. Experiment by J. Richardson. See Percy's Metallurgy, Iron and Steel, p. 150. 2670. Alloy of 2 of copper with 8 of iron. 800 grains of iron and 200 grains of copper were melted together as before ; the button was well melted with a loss of only 2 grains. It is extremely brittle. It has a pale coppery grey colour, and is crystalline granular. The fracture shows iron-grey mica-like scales, intermingled with copper-red particles. It contains 80 per cent, of iron. Experiment by J. Richardson. See Percy's Metallurgy, Iron and Steel, p. 140. 2671. Alloy of iron and manganese. Made by G. Parry, Ebbw Yale Iron Works. It has a coarsely crystalline fracture, is greyish white, and is said to contain about 20 per cent, of manganese. 2672. .Alloy of iron and manganese. Obtained by reducing together haematite and pyrolusite. It probably contains carbon derived from the reducing agent. 2673. Alloy of iron and manganese. Obtained by melting together spiegeteisen^ which already contains some manganese and carbon, with pyrolusite to increase the proportion of manganese. 2674. Alloy of iron and manganese, and containing carbon. 303 2675. Ferromanganese crystals. Made under the direction of Mons. Th. Gautier, in Wales, at the Pyle Company's Works, 1885. It is a loose aggregation of small crystals, some of which are acicular and iridescent. They contain 86 per cent, of manganese. 2676. Alloy of iron and tin. 490 grains of iron have been melted with 10 grains of tin, producing an alloy containing 2 per cent, of tin. The resulting button is brittle, being cracked in several places. 2677. Attempt at the union of iron and titanium. 125 grains of prepared ferric oxide and 127 grains of rutile were ex- posed in a covered brasqued crucible during 1J hours, to a white heat, and reheated with 40 grains of lime and 60 grains of glass. Some grey globules are produced, but these, on analysis, do not show a trace of titanium. 2678. Alloy of titanium and iron. A piece of rolled sheet iron, made direct from ilmenite, containing 45 per cent, of titanic acid, the remainder being iron oxides and only half per cent, of lime and magnesia. The whole of the metal was reduced. It COE tains the two elements in probably about equal proportions. Communicated by J. D. Clure, of Handsworth, 1875. 2679. Alloy of iron and antimony. It contains 70 per cent, of antimony and 30 per cent, of iron. It its a porous ingot, tarnished on the fracture. 2680. Attempt at the union of iron and bismuth.- 50 grains of bismuth have been melted together with 150 grains of iron. The bismuth has been for the mcst part eliminated, the resulting metal containing only 2-23 per cent, of bismuth. 2681. Union of iron and bismuth. 290 grains of iron have been fused with 10 grains of bismuth, under glass. The resulting button shows a loss of one grain only. Experi- ment by W. B. Richardson. 2682. Alloy of iron with 1 per cent, of nickel. 495 grains of iron were melled, under glass, with five grains of nickel. A well melted button has been obtained, weighing 490 grains. The fracture is like that of iron alone. Experiment by W. B. Richardson. See Percy's Metallurgy, Iron and Steel, p. 171, No. 1. 2683. Alloy of iron with 5 per cent, of nickel. 285 grains of iron were melted, under glass, with 15 grains of nickel. The button weighs 290 grains, and is coated with black scale. It is more brittle than iron, and has a loose granular fracture and bright colour. Experiment, by W. B. Richardson. See Percy's Metallurgy, Iron and Steel, p. 171, No. 2. 304 2884. Alloy of iron with 20 per cent, of nickel. 240 grains of iron were melted, under glass, with 60 grains of nickel. The button weighs 280 grains. Its surface is smooth and is free from scale. It is brittle and has a very irregular fibro-columnar fracture. It is bluish- white, and has a specific gravity of 7 -91 7. Experiment by W. B. Eichardson. See Percy's Metallurgy, Iron and Steel, p. 171, No. 3. 2685. Alloy of iron and nickel in equal parts. 200 grains of each metal were melted together, under glass. The resulting button weighs 380 grains. It is smooth, free from scale, and tarnishes yellow. It is very brittle. It has a uniform, even, finely granular fracture, with minute crystalline faces. Its specific gravity is 8-2. Experiment by W. B. Eichardson. See Percy's Metallurgy, Iron and Steel, p. 172, No. 4. 2686. Experiment on the alloying of iron with cobalt. 200 grains of nearly pure haematite and 200 grains protoxide of cobalt were mixed and placed in a charcoal-lined plumbago crucible, the cavity being filled up with a mixture of china clay and lime, the pot luted over, and the whole exposed to a white heat for two hours. The result is a well fused button weighing 296 grains, attracted by the magnet. It flattened under the hammer and then broke. The fracture is granular, bluish-grey, with feeble lustre. It is accompanied by melted globules and a pale bluish-green glassy slag. It contains 46*71 per cent, of iron, and the remainder is cobalt. Experiment by E. Smith. See Percy's Metallurgy, Iron and Steel, p. 173. 2687. Second experiment on the alloying of iron with cobalt. 360 grains of nearly pure hematite and 40 grains of cobalt oxide were treated in the same way as in the last experiment. The result is a well fused button weighing 286 grains, attracted by the magnet. It has broken under the hammer. The fracture is granular, greyish-white in the centre, and on the outside is a very thin, fine-grained, dull, dark- grey layer. There are fewer globules, and a similar slag. It contains 87 '21 per cent, of iron. Experiment by E. Smith. See Percy's Metallurgy, Iron and Steel, p. 173. 2688. Alloy of iron with 5 per cent, of aluminium. 950 grains of wrought iron were melted, and 50 grains of metallic aluminium were plunged in and stirred. The union of the metals seems here imperfect, and the whiter portion is so brittle as to be crumbling. Experiment by E. Smith. 2689. Experiment on the alloying of iron and magnesium. 140 grains of iron were melted with 20 grains of magnesium. The button weighs 160 grains. It has a rough, crystalline, granular fracture ; does not yield very readily to the hammer. 2690. Alloy of iron and magnesium. 2691. Alloy of iron and magnesium. On analysis it yields only a trace of magnesium, carbon, and silica. 305 2692. Alloy of iron and tungsten, containing 9 5 per cent, of tungsten. The complete analysis shows Carbon - - - 1-123 Tungsten - - 9-477 Silicon - - 0-756 Manganese - 0-520 Tron .... 88-124 100-000 It contains no sulphur or phosphorus. In its present state it can be cut by a file; nut after heating to red heat' and quenching in water, it becomes much harder, and cannot be touched by a file. It has an exceedingly fine granular fracture. Analysed and communicated by W. Baker, 1874. 2693. Tungsten steel, said to contain 4 per cent, of tungsten. Made by adding wolfram to molten steel. From Messrs. Seebohm and Co.'s Works, Sheffield. It has a fine silky fracture. 2694. Tungsten steel. Manufactured at Siemens' Steel Works, Landore, 1870. It has a granular fracture, and possesses great power of retaining magnetism. 2695. Tungsten steel from Austria. Exhibited at the Congress of Miners in Vienna, 1858. The fracture is remarkably fine, uniform, compact, and conchoidal. Not favourably reported on as to its working and other qualities by Mr. Saunderson, of Sheffield. Communicated by W. W. Smyth. See Percy's Metallurgy, Iron and Steel, p. 193. 2696. Experiments on the alloying of iron with chromium. Experiment I. In all four experiments nearly pure red hasmatite was used, and pre- pared sesquioxide of chromium. The quantities were intimately mixed and placed in a charcoal-lined French crucible, the cavity filled up with charcoal powder, the whole luted over, and exposed to a white heat for two hours. In this first experiment 190 grains of hasmatite and 10 grains of chromium oxide were employed. The result is a well fused button with globules, and interlacing crystals on the surface. The fracture is white, bright, and crystalline. It is hard, and contains 4-24 per cent, of chromium. See Percy's Metallurgy, Iron and Steel, p. 187. Experiment by R. Smith. 2697. Alloying of iron and chromium. Experiment II. 150 grains of haematite and 50 grains of chromium oxide were taken. The result is a well fused button with globules, which is hard, brittle, with a tin-white, very bright, and finely granular fracture. It is crystal- line in structure, and contains 72-93 per cent, of iron. See Percy's Metallurgy, Iron !ind Steel, p. 187. U 61955. TJ 306 2698. Alloying of iron and chromium. Experiment III. 150 grains of haematite and 150 grains of chromium oxide were taken, and half as much carbon was added more in the form of anthracite powder instead of charcoal. The result is a somewhat spongy button with metallic globules, not attracted by the magnet, hard, and with a finely granular, bright, greyish- white fracture. It contains 45 35 per cent, of iron. A slag is also produced in this case. See Percy's Metallurgy, Iroft and Steel, p. 187. 2699. Alloying of iron and chromium. Experiment IV. 50 grains of hematite and 150 grains of chromium oxide were taken. The result is an imperfectly fused spongy mass less coherent than the last. It is not attracted by the magnet, is very hard, and can be crushed. The colour is yellowish-grey, and the lustre rather dull. In the centre are bright needle-shaped crystals. It contains 23-42 per cent, of iron. See Percy's Metallurgy, Iron and Steel, p. 187. 2700. Alloy of chromium and iron made by the reduction of chromium oxide in the electric furnace. It contains 14 per cent, of chromium and the remainder is iron. It has rusted on the fractured surface. For the " electric furnace," see No. 2405. 2701. Alloy of iron containing 5 per cent, of chromium. It has a largely crystalline fracture and a greyish colour. 2702. Alloy of iron containing 10 per cent, of chromium. It has a crystalline fracture and a whitish colour. It is hard enough to scratch glass. 2703. Alloy of iron containing 20 per cent, of chromium. It has a crystalline fracture, with numerous narrow crystals, and is of a whitish colour. It scratches glass easily. 2704. Alloy of iron containing 30 per cent, of chromium. P This has a vesicular structure, being largely composed of brilliant, prismatic, interlocking crystals, with intervals between. The colour is white. It scratches glass with difficulty. 2705. Alloy of iron containing 40 per cent, of chromium. It is finely vesicular, having an almost granular fracture, and a rather dull colour. It does not scratch glass. 2706. Chromium steel. A sample of normal steel containing 0-90 per cent, of carbon, and a rod of chromium steel containing 5 95 per cent, of chromium, and 308 of silicon. Communicated by C. V. Boys. SPECIAL CASES OF THE REDUCTION AND CEMENTATION OF IRON. 2707. Clay ironstone cemented in charcoal. No reduction has taken place. Prepared in the Metallurgical Laboratory of the Royal School of Mines. 307 2708. Haematite cemented in charcoal powder. This is at the same time reduced to a ma;>s of iron, which retains the kidney shape, the concentric layers and the radiating lines of the original ore. Prepared in the Metallurgical Laboratory of the Royal School of Mines, 2709. Cumberland haematite reduced direct. This is a mass of iron, which retains the shape, and the concentric and radiating structure of the original ore, which has parted by open cracks. Communicated by R. Mushet, 1866. 2710. Red iron ore reduced by cementation in charcoal. Communicated by S. Blackwell, 1867. This has the same appearance as the last, but is tinged with blue. 2711. Powdered clay iron ore reduced by means of charcoal. A stick of charcoal has been placed in the centre of a retort, and surrounded by the powdered ore ; this has been closed and heated. The result is a very porous, mostly metallic, iron mass. Prepared in the Laboratory of the Royal School of Mines. 2712. Accidental reduction of iron by coke. A piece of coke has been imbedded by chance in the top cinder while the latter was being heated. The spot where it lay is now surrounded by a thin irregular sheet of reduced iron. 2713. A series of specimens illustrating the carburisation of ore by means of the furnace gases. No. 1. .The calcined ironstone which was exposed to the furnace fumes. It is derived from the Cleveland iron ore. No 2 is the same after exposure to the 'escaping gases of a furnace 48 feet high for 24 hours. No. 4 is another sample of calcined Cleveland ore, containing 42 '2 per cent, of iron. No. 3 is this sample after it has been subjected to the gases of a furnace 80 feet in height for 24 hours. EXPERIMENTS ON METEORIC IRON. Conducted by R. Smith, on portions of the largest meteorite in the British Museum and on the rust derived from it. 2714. Pieces of the meteoric iron as received. They are all small fragments, and are mostly changed to ferric oxide. They exhibit a pseudo-columnar structure. 2715. Meteoric iron. Rusted portion reduced by carbonic oxide gas. The material has been heated in a crucible placed within another and filled up with anthracite powder. The result is that irregular metallic masses are produced, black on the surface, purplish-white within, and showing an irregular, prismatic structure. 2716. Meteoric iron. Rusted portion reduced by hydrogen gas and cooled in the same. Experiment I. It forms irregular, prismatic, metallic masses of purplish hue. % U 2 308 2717. Meteoric iron. Rusted portion reduced by hydrogen. Experiment II. It was heated in hydrogen for two hours and left to cool for two hours more in hydrogen. The result is very similar to the last, but the lustre is a little more brilliant. 2718. Meteoric iron. Rusted portion reduced in hydrogen and afterwards remelted. A portion was selected showing Wiedmanstattian figures, and this was fused under glass and allowed to cool in the furnace. The arborescent, crystalline structure is now well seen on the surface and top of the melted button, which has a coarse crystalline fracture. 2719. Meteoric iron. Metallic portion melted under plate glass and allowed to cooi in the furnace. It weighs 1,292 grains. The fracture is granular, and the crystalline structure of the surface so minute as to be almost invisible. 2720. Meteoric iron. Metallic portion melted under glass, and allowed to cool in the furnace. Second experiment. The button weighs 1,,'ViO grains, and the whole of the surface is covered by arborescent crystallisation. 2721. Meteoric iron. Metallic portion melted under glass, and allowed to cool in the furnace. Third experiment. The fracture is finely granular, and no crystallisation is visible on the surface. 2722. .Meteoric iron, run into moulds and hammered. Made from the rusted portion after reduction by cementation in charcoal. IRON OHES. BRITISH. Magnetic Iron Ores. 2723. Magnetic iron ore from Rosedale, Yorkshire. This is a black mass, belonging to the base of the Inferior Oolite. It is oolitic in structure, and appears to have been primarily calcareous. Then the lime was replaced by iron, and, finally, the carbonic acid has, for the most part, escaped. It is mixed with some clay. Analyzed by E. F. Techmacher. Oxide of iron Alumina Silica Lime - Magnesia Water and loss 100-00 This gives a per-centage of 55 of metallic iron. 309 2724. Magnetic iron ore from Rosedale, Yorkshire. Another portion of the same mass, assaying only 41 '5 percent, of iron. 2725. Magnetic iron ore from Rosedale, Yorkshire. From the south drift. A blue -black variety, containing 39 "38 per cent, of metallic iron. Communicated by A. C. Sheriff. See Percy's Metallurgy, Iron and Steel, p. 235. 2726. Magnetic iron ore from Rosedale, Yorkshire. From the old drift. A bluish dark grey variety, containing 38*44 per cent, of metallic iron. Communicated by A. C. Sheriff. See Percy's Metallurgy, Iron and Steel, p. 235. 2727. Magnetic iron ore from Limerick. A concretionary mass, partly weathered to brown oxide. 2728. Magnetic iron ore from near Torquay, Devonshire. A crystalline vein-substance, probably in Devonian rocks, accompanied by fibrous hornblende. Yields 58 93 per cent, of metallic iron. 2729. Magnetic iron ore from Dolgelly, N. Wales. A fine grained, crystalline vein substance, probably* in Cambrian rocks, in which brilliant octahedra of magnetite may be seen. Analysed by W. J. Ward. It contains 41 '58 per cent, of metallic iron, 0'29 per cent, of phosphorus, and 0*17 per cent, of sulphur. There is an in- soluble residue of 25 * 76 per cent, and a loss on ignition of 3*92 .pet- cent. Communicated by Brassey and Co., 1867. Hcematites. 2730. Micaceous iron ore from Cornwall. Obtained from a fissure. It contains 77 '20 per cent, of ferric oxide, equivalent to 54*03 per cent, of metallic iron. Only a small portion of the powder is taken up by the magnet. Analysed by R. Smith. Com- municated by Mr. Murray. 2731. Micaceous iron ore from Wadebridge, Cornwall. A concretionary mass with radiating crystals of black oxide passing, to red kidney ore. Used at Blaiua Ironworks in 1859. 2732. Specular iron ore from Birkershanon, Eskdale. Communicated by F. H. Noyes. 2733. Kidney iron ore from the New Vein, Birkershanon, Eskdale. Communicated by F. H. Noyes. 2734. Micaceous iron ore from Bovey Tracey, Devonshire. A brittle mass, going down into powder of purplish tint. It contains 57*57 per cent, of metallic iron. 310 2735. Micaceous iron ore from Devonshire. Communicated by D. Pridham, 1867. Similar to the last. Occurs as a vein in the Devonian rocks. 2736. Earthy red haematite from Somersetshire. Contains 46*03 per cent, of metallic iron. It forms part of the Dolomitic Conglomerate of the Trias. Communicated by R. Bristowe. 2737. Iron ore from Luccombe, Somerset. This is a sandstone of the Trias, deeply impregnated with ferric oxide between the grains of sand, and forms part of the Dolomitic Conglome- rate. Communicated by R. Bristowe. 2738. Haematite from Luccombe, Somerset. This is more or less in the micaceous form. It consists of a breccia, in tfye Triassic rocks, which had the interstices infiltrated by the ferric oxide. It contains therefore many fragments of stone, and .forms part of the series called the Dolomitic Conglomerate. Communicated by R. Bristowe. 2739. Ironstone from the Trias of Luccombe, Somerset. Fragments of stone imbedded in an abundant matrix of red haematite, and forming part of the Dolomitic Conglomerate. Communicated by R. Bristowe. 2740. Kidney ore from Cleator, Whitehaven, Cumberland. Communicated by M. Blackwell. 2741. Red -and black kidney ore from Ulverstone, Lanca- shire. 2742. Puddling ore from Ulverstone. This is most suitable for putting on the bottoms of puddling furnaces. Communicated by Mr. Roper, Newland furnace. 2743. Blast ore from Ulverstone. This is not so suitable for puddling, but is used in the blast furnaces. Communicated by Mr. Roper. 2744. Gravelly iron ore from Ulverstone. All these ores from Ulverstone and Cleator occur in fissures and nests in the Carboniferous Limestone. 2745. Five samples of varieties of haematite iron ore in powder. As used by the Whitehaven Haematite Iron Co. 2746. Haematite iron ore as used at Dowlais Furnaces, 1870. 2747. Another more earthy variety of haematite used at Dowlais Furnaces, 1870. 2748. Haematite from the Mumbles, Swansea. Contained in a slickensided vein in the Carboniferous Limestone. 311 2749. Dark haematite from the Forest of Dean. This is a very solid mass of fine grain, weathering red, of concentric structure and conchoidal fracture. 2750. Iron ore from Ashton-under-Lyne. Doubtless from the Trias. It is a red, earthy, fissure-material with cavities, and contains sulphate of barium. Communicated by E. Riley, Dowlais. 2751. Haematite from Winsford, Somerset. A compact, earthy, red mass, with geodes of quartz crystals. In the mountain limestone of the Mendip Hills. 2752. Haematite from Ilfraeombe, North Devon. A radiating concretionary mass containing 82 64 per cent, of ferric oxide, equivalent to 57 84 per cent, of metallic iron. 2753. Iron ore from the Carboniferous Limestone of Pembrokeshire. This consists of models in haematite of numerous organic remains which were of course originally composed of carbonate of lime, which has been replaced by the iron oxide. Portions of Encrinites and of Bryozoa have been detected in it by J. W. Salter. 2754. Iron ore from the " Crane " Iron Works. This consists of a cavernous mass, with long, parallel, hollow spaces, round which the ferric oxide is accumulated, covered with red powder. 2755. Iron ore quarried near Berry Head, Tavistock, on .the shore and inland. Massive haematite, partially converted into limonite. Brown ffcematites. 2756. Iron ore from Tynardreath, Par Station, Cornwall. Banded vein-stuff, containing 63-31 per cent, of metallic iron. Communicated by Wm. Polkinghorne. 2757. Iron ore from Tynardreath, Par, Cornwall. Dark crystalline material with fragments. Contains 43-88 per cent, of metallic iron. 2758. Brown iron ore from Ilsington, Devon. Irregular, tubular masses of dark limonite. Used at the Atlas Iron Works, Bovey. Communicated by W. W. Smyth. 2759. Brown iron ore from the Brendon Hilis, Somerset. A dark, irregular, porous, banded mass, used at the Ebbw Vale Iron Works, 1859. Associated with spathic ores in the Devonian slates. 312 2760. A mixed ore from the mines at Perran, Cornwall. Analysed by W. J. Ward. Ferrous oxide - Ferric oxide - Manganous oxide Alumina Lime - Magnesia Phosphoric acid Sulphur Carbonic acid - Silica - Water - 99-40 This is equivalent to 34-07 per cent, of metallic iron. An irregular, breccia-like spathose rock. 2761. Brown iron ore from Perran Iron Mines, Cornwall. Porous concretionary masses. Analysed by W. J. Ward, 1870. Ferric oxide Manganous oxide Alumina Lime - Magnesia Phosphoric acid Sulphuric acid - Silica - Water - 99-74 This is equivalent to 52-45 per cent, of metallic iron. 2762. Brown haematite from Froghall, near Cheadle, Staffordshire. It is a calciferous brown haematite, occurring in the latest portion of the Coal Measures. It is compact, homogeneous, and brownish-red in- colour and has a vein of calcareous spar. Analysed, when dried, by A. Dick. Iron oxide Manganous oxide Lime - Magnesia Carbonic acid - Phosphoric acid Sulphuric acid - Combined water Organic matter Ignited insoluble residue 98-78 See Percy's Metallurgy, Iron and Steel, pp. 207, 224. 313 2763. Brush iron ore, Forest of Dean A concretionary solid brown ore. For analyses of these so called ores, see Percy's Metallurgy, Iron and Steel, p. 207. One variety contains 90 per cent, of ferric oxide. It is derived from the Coal Measures. 2764. Forest ore, or Smith ore, Forest of Dean. An earthy brownish-red gravelly ore, derived from the Coal Measures. An analysis of this ore, but not, of this sample, by A. Dick, gave 89-76 per cent, of ferric oxide, with 7 per cent, of water, and fractions of the usual bases arid of phosphoric acid. See Percy's Metallurgy, Iron and Steel, p. 207. 2765. Forest of Dean ore Used at the Dowlais Iron Works, 1870. A tufaceous mass with small parallel hollows. 2766. Botryoidal and stalactitic brown haematite from the Forest of Dean coal measures. Massive within and with radiating crystals on the surface. 2767. Iron ore from the Forest of Dean, ground and prepared as a red colouring matter. 2768. Iron ore from the Fore.st of Dean, ground and prepared as a brown colouring matter. 2769. Bog iron ore, from Ireland. A solid irregular mass, in parts nearly black. 2770. Aluminous iron ore from Antrim, north of Ireland. A dark, reddish-brown granular mass, with black pebbles. It has a specilic gravity 2-9, and contains 40-49 per cent, of metallic iron. Communicated by Mr. Bauerman. Compare the analyses, p. 207 of Percy's Metallurgy, Iron and Steel. 2771. Aluminous iron ore from Belfast. Used at the Dowlais Iron Works, 1870. It consists of a breccia of darker red fragments in a light red matrix and is entirely soft and earthy. 2772. Iron ore from Arklow, Ireland. Used at the Dowlais Iron Works, 1870. Consists of a porous, dark, concretionary mass. 2773. Iron ore from the north of Ireland. A red earthy ma^s, which yielded on analysis, ferric oxide, 59-08; alumina, 27-30; silica, 8-80. The loss on calcination was 6-86 per cent, and the ignited insoluble residue, 21 37 per cent. There is 41-36 per cent, of metallic iron. These ores occur in lenticular beds, asso- ciated with the dolerites of Antrim and are of Tertiary age. 2774. Iron ore from the north of Ireland. A brownish red earthy soft mass. Yielding on analysis 35-20 per cent, of ferric oxide, 38-22 of alumina, 6-06 of silica. The loss on 314 calcination is 24 26, and the ignited insoluble residue is 24 90. This yields 24-64 per cent, of metallic iron when raw, 31-29 when calcined. 2775. Iron ore from the north of Ireland. A dark irregular earthy mass of various red and brown colours, yield- ing on analysis 77 84 per cent, of ferric oxide, 2- 16 of ferrous oxide, 7-16 of alumina, 11-92 of silica. The loss on ignition was 3-24 per cent, and the ignited insoluble residue was 20 '31. This yields 56-17 per cent, of metallic iron. None of these three ores contain any sensible proportion of phosphorus or sulphur. 2776. Northampton iron ore. Used at the Dowlais Iron Works, 1870. An earthy hydrated sesquioxide of iron, oolitic in structure and ochre-brown in colour. More or less concretionary. It belongs to the lower part of the Inferior Oolite. These ores contain about 51 per cent, of ferric oxide with 14 per cent, of insoluble residue. It was one of these specimens of Northamp- ton iron ore to which Dr. Percy directed the attention of Mr. Blackwell, of Dudley, and thus led to its introduction Jnto extensive use. See Phillip's Ores and Ore Deposits, p. 172. 2777. Northampton iron ore. Used at Dowlais Jron Works, 1870. This is a vacuous ore, from which all the calcareous particles have been dissolved, leaving minute hollow spaces separated by the insoluble ferric oxide. 2778. Northampton iron ore showing the origin of the ferric oxide by the weathering of the carbonate. Both parts are of oolitic structure. The interior is bluish green, the outside shows a concretionary deposit of ferric oxide. In Dr. Percy's Metallurgy, Iron, ana Steel, p. 209, are given analyses by A. Dick of the inner and outer portions of this or a similar specimen. They are Outer part. Inner part. Ferric oxide - - 38-04 Ferrous oxide - 10 .54 . 33-29 Manganese oxide - 0-69 1-11 Alumina - 12-35 4-62 Lime - - - trace 0-52 Magnesia - 4-13 7-96 Silica - 1-96 1-99 Carbonic acid - - 0-16 24-79 Phosphoric acid 0-26 0-22 Iron bisulphide - 0-13 0-13 Water (combined) - 6-92 0-54 Organic matter 0-19 0-08 Insoluble residue - 24-61 . 24 '07 99-98 99-32 2779. Series of specimens (5) of " iron ore " from Ban bury. These belong to the Marlstoue of the Middle Lias. They cannot be regarded as iron ore properly so called, as the sample analysed by A. Dick (see Percy's Metallurgy, Iron and Steel, p. 209) gave only 3-19 for ferric oxide and 12-34 of ferrous oxide. 315 2780. Iron ore from a seven foot bed " at Thirsk, Yorkshire. This is an oolitic carbonate mostly converted into hydrated sesqui- oxide of iron. It belongs to the lower part of the Inferior Oolite. 2781. Vanadium compound obtained from Westbury iron ore. It is a green amorphous powder. The Westbury iron ore is an oolitic deposit belonging to the Upper Oolites. Communicated by E. Biley, 1881. 2782. Oolitic iron ore from the Tealby Series, Lincolnshire. This belongs to the Middle Neocomian series. It is composed of black grains of hydrated ferric oxide imbedded in an earthy matrix of similar material. Analysed by W. J. Ward in 1873. Yields 27-83 per cent, of metallic iron. f 2783. Iron ore from East Cliff, Hastings. A nodular concretion from the Wealden clays, similar to those once smelted in Kent and Sussex. 2784. Earthy brown haematites from Alston Moor. Various superficial masses produced by weathering vein-stuffs, and forrning a gossan. Analysed by Dr. Percy in 1848. 2785. Impregnation of wood (!) by hydrated ferric oxide, at Alston Moor, with small crystals of baryta. 2786. Brown hsematite from Llantrissant, Glamorganshire. From a remarkable deposit forming in the base of the Magnesian con- glomerate and resting on the Carboniferous Limestone. Analysed by E. Riley, gives 59 05 per cent, of ferric oxide, 34 40 per cent, of silica, 6 '14 of combined water and fractions of manganous oxide, lime, magnesia, phosphoric acid, and pyrites, and yields 41-34 per cent, of metallic iron. This specimen, however, contains a fair amount of calcite. 2787. Clay ironstone from the Wealden on the shore near Hastings. Red on the surface by weathering to ferric oxide, reddish-brown within where unweathered, and with root-like markings coloured green as by iron carbonate. 2788. Ironstone from the Upper Eocene clays of Christ- church, Hants. ' A fine-grained sandy mass. Smelted at Ebbw Vale Iron Works in 1865. Spathic Iron Ores. 2789. Spathic iron ore from Cornwall. A compact, finely crystalline mass. Communicated by Mr. Cony- beare. 316 2790. Spathic iron ore from the Brendon Hills, Somerset- shire. A coarsely crystalline mass of characteristic brownish tint. It occurs as a vein in the Devonian series, and is, or has been, much worked by the Ebbw Vale Iron Company. Dr. Percy (Metallurgy, Iron and Steel, p. 210) gives an analysis of this ore showing 43-84 of ferrous oxide, 12-64 of manganous oxide, 3-63 per cent, of magnesia, and 38-86 per cent, of carbonic acid. This corresponds to 34-67 per cent, of metallic iron. 2791. Spathic iron ores from the Brendon Hills, Somerset, assayed from iron, showing variety of yield. Analysed by W. J. Ward, 1873. No. 1, taken from the ore as delivered at the Ebbw Va.le Iron Works, yields 33-87 per cent, of metallic iron. No. 2, from the same lode, two miles west of Lockyard, yields 27 '32 per cent. No. 3, from the same lode, taken as delivered at the Ebbw Vale Iron Works, yields 33-96 per cent. No. 4, in a partially decomposed state by which the carbonate has partly become oxide, yields 35 27 per cent. These ores are specially employed for the manufacture of spiegeleisen. 2792. Spathic iron ore from the Brendon Hills, Somerset, containing patches of copper pyrites. 2793. White spathic iron ore from Perran, Cornwall. A compact, finely crystalline mass from a band in the Devonian slates. Analysed by W. J. Ward, 1870. Ferrous oxide Ferric oxide - Manganous oxide Alumina Lime Magnesia Phosphoric acid Sulphur Silica Carbonic acid - Water 99-40 This is equivalent to a yield of 35-67 per cent, of metallic iron. 2794. Spathic iron ore from Devonshire. A finely crystalline mass, containing 73-41 per cent, of ferrous carbonate and 18 -22' per cent, of manganous carbonate, which is equivalent to 35-44 per cent, of metallic iron and 11-25 per cent, of manganous oxide. Communicated by Sir Lawrence Palk. 2795. Spathic iron ore from Co. Fermanagh, Ireland. A breccia! ed mass, with a concretionary coating of hydrous ferric oxide. The interior is mottled white and dark green. This inner portion, assayed by R. Smith, gives 74-41 of ferrous carbonate, which is equivalent to 35-92 per cent, of metallic iron. 317 2796. Spathic iron ore from Weardale, Durham. A coarsely crystalline mass, forming a vein in the Carboniferous Limestone. A specimen (? this one) from this lode, analysed by C. Tookey, gave per cent. 49-77 of ferrous oxide, 37-20 of carbonic acid, 3-96 of lime, and 2-83 of magnesia. This is equivalent to 38-95 per cent, of metallic iron. 2797. Spathic iron ore from Great Ormes Head, North Wales. On the west side, near the level of the copper mine, from an old dressing floor on the shore, probably forming the gangue of the copper vein, as in No. 2792. 2798. Spathic iron ore from Llandudno. It occurs in a vertical cleft or fissure, and is accompanied by soft ochre-like stuff, derived from its decomposition into a brown haematite. 2799. Crystalline chalybite formed on the surface and fissures of a septarium of red haematite. From Wadebridge, Cornwall. Used at the Blaina Iron Works, 1889. The crystals are well-formed rhombs. 2800. " Balls " iron ore. Used at Russell Hall's furnaces, Dudley. It consists of the usual argillaceous iron ore of the coal measures, coated over with sheets and little tufted crystals of chalybite. In one specimen it is associated with pyrites similarly disposed. 2801. Spathic ore on the surface of the fissure of a septarium of Welsh clay-ironstone. Used at Ebbw Vale Iron Works, 1865. 2802. Mass of quartz in the midst of spathic iron ore which lias not been picked out as it ought to be from the material to be smelted, showing the accidental source of some irregu- larities in working the ore. Argillaceous Ores. 2803. Cleveland iron ore. This is from the main seam, belonging to the Middle Lias. It is a bluish -green oolitic rock in which many of the original grains have been converted into earthy carbonate of irou, which is much mixed with impurities. As analysed by A. Dick it yields 39-92 per cent, of ferrous oxide, 22-85 of carbonic acid, with considerable amounts of alumina, lime, and silica, the total iron being 33-62 per cent. See Percy's Metallurgy, Iron and Steel, p. 221. 2804. Earthy iron ore from Duston, Northamptonshire This belongs to the lower part of the Inferior Oolite, and by weathering produces the surface ores, Nos. 2776-8- It is an oolitic rock, originally calcareous, and now for the most part converted into an 318 impure carbonate of iron. Assayed by R. Smith, and yields 38-13 per cent, of metallic iron and 1 -85 per cent, of phosphoric acid. 2805. Black-band ironstone from Llynvi Coal and Iron Company. This is a black argillaceous band in the South Wales Coal Measures. It contains 34 per cent, of metallic iron, in the form of admixed carbonate. 2806. Another sample of black-band ironstone from the Llynvi Coal and Iron Company. This contains 35-22 per cent, of metallic iron. Both analysed by W. J. Ward, 1868. 2807. Bedded ironstone, called " Caus-y-glo," Ystalyfera. This is one of the best quality. A sample which corresponds to this in description analysed at the Woolwich Arsenal gave 33-45 per cent, of metallic iron. It is from the Coal Measures of South Wales. 2808. Septarian ironstone, called " Coed folde," Ystalyfera. From the South Wales Coal Measures. This is also called " white mines " or " balls and pins," this specimen being from one of the balls. The two united were analysed by A. Dick and found to contain 29 34 of ferrous oxide, 25-56 of carbonic acid, and 35-73 of insoluble residue, or 23-22 per cent, of metallic iron. See Percy's Metallurgy, Iron and Steel, p. 220 ; and Iron Ores, of Great Britain, Part III., p. 212. 2809. Pennystone ironstone, Ystalyfera, South Wales. This is a small flat nodule of argillaceous ironstone, occurring separately in the Coal Measure clays. 2810. Argillaceous ironstone from Bedworth, near Coventry, Warwickshire. A reddish rock in the Coal Measures. Analysed in 1846 by Dr. Percy. It yields Ferrous oxide - Manganous oxide Alumina .... Lime - Magnesia - - Silica Carbonic acid Phosphoric acid Water 100-00 See Percy's Metallurgy, Iron and Steel, p. 217. 2811. Argillaceous ironstone, called Welsh Mine, Dowlais, Glamorganshire. There are numerous beds included under this head, some named the Little Blue vein, others the Lumpy vein, of which analyses by 319 E. Riley, at Dowlais, are given by Dr. Percy, Metallurgy, Iron and Steel, p. 218. This appears to belong to the Lumpy vein, which contains 34-72 per cent, of metallic iron. 2812. " Welsh Mine " iron ore, calcined before smelting. From the Dowlais Iron Works, 1 870. 2813. Clay ironstone from the Coal Measures, Moreton Colliery, near Tenby. It is part of a septarian nodule. 2814. Hatchettine from Merthyr Tydvil, Glamorganshire. A soft, easily fusible mineral, allied to the paraffins, occurring in the crevices of the clay ironstone in this, the original, locality. See Conybeare, Ann. Phil. Vol. 1, p. 136, 1822. 2815. Llwynenion ironstone, British Iron Company's Works, Ay re Fair, Ruabon, Denbighshire. A fine-grained, reddish, argillaceous mass from a nodule. 2816. Ironstone of the " stone " coal, Ayre Fair, Ruabon, Denbighshire. This is black, and contains remains of Anthracosia. It is considered the best in the district. Communicated by W. W. Smyth. 2817. Llwynenion ironstone, lower seams, Ayre Fair, Ruabon, Denbighshire. This is darker than the last. 2818. "Blue Flats" ironstone from Somerford Colliery, South Staffordshire. An ironstone of very limited geographical range, only between Wolverhampton and Walsall. It consists of flat beds ; one of these pieces shows the remains of Calamites, the other of Productus, being part of a nodule weathering a purplish blue. This measure has been analysed by C. Tookey, and yields ferrous oxide 42-34 per cent., carbonic acid 30-91, and insoluble residue 15-50, being equivalent to 34-41 per cent, of metallic iron. See Percy's Metallurgy, Iron and Steel, p. 215. 2819. " Cranstone " ironstone, Madeley, Shropshire. This is the lowest in the district, and occurs in the form of nodules. A specimen of this ore has been analysed by J. Spiller, and gives ferrous oxide 51-45, carbonic acid 33-31, and insoluble residue 9-60, equivalent to 40 27 per cent, of metallic iron. See Percy's Metallurgy, Iron and Steel, p. 218. 2820. Pennystone ironstone, Madeley, Shropshire. A small concretion of reddish clay ironstone, with a septarian centre. A specimen of this ore has been analysed by J. Spiller, and yields ferrous oxide 44-19, carbonic acid 32-02, insoluble matter 13-50, equivalent to 34-75 per cent, of metallic iron. See Percy's Metallurgy, Iron and Steel, p. 218. 320 2821. Nodular form of the Pennystone ironstone, Madeley, Shropshire. 2822. Clay ironstone, employed at the Newland furnaces, Ulverstone. Lancashire, for mixing with the haematite ores to form a slag. 2823. Earthy iron ore from Co. Fermanagh, Ireland. A rough solid mass. Analysed by R. Smith.. It contains 75-92 per cent, of ferrous carbonate, equivalent to 36-65 per cent, of metallic iron, and 11-40 per cent, of manganous carbonate, equivalent to 7-04 per cent, of manganous oxide. 2824. Calcined iron ores from Co. Fermanagh, Ireland. Analysed by R. Smith, contains 29-83 per cent, of metallic iron. 2825. Brown iron ore from co. Fermanagh, Ireland. An earthy nodule with dense coating. Analysed by R. Smith, con- tains 38-97 per cent, of metallic iron. It loses 18-33 per cent, on calcination. 2826. Clay iron ore from South Staffordshire, containing blende and iron pyrites. The blende is in considerable crystalline masses in the centre of the ironstone nodule and is sprinkled with mamillse of iron pyrites. 2827. Nodule of clay ironstone, containing massive iron pyrites in large crystals. 2828. Iron ore from Wales. It is black, shaley, and. oolitic. Probably it is the pisolitic iron ore characteristic of the lower part of the Silurian series. 2829. Massive oolitic iron ore from the Silurian series of Carnarvonshire. 2830. Carbonaceous clay ironstone called "Duffryn Brass." J)owlais, South Wales. A brownish -grey stone called by this name, analysed by E. Riley, was found to contain 58-48 per cent, of carbonate of iron and 8 -95 per cent, of coal. See Percy's Metallurgy, Iron and Steel, p. 203. This is composed of minute fragments of coal set in a black earthy paste. 2831. Clay ironstone septarian nodule, coated along the cracks with pearl spar in rhombs and sprinkled with copper pyrites in double pyramids. From Somerford Colliery, near Wolverhampton. 2832. Clay ironstone, containing galena in the form of a slight incrustation. From the "Wall and Bench" Coal, Ayre Fair Works, Ruabon, Denbighshire. 321 2833. Piece of weathered clay-ironstone, showing the con- version of blue carbonate into the brown hsematite on the surface. By a ruined blast furnace. Melincourt Fall, Resolven, near Neath. 2834. Iron ore from the upper part of the Lower Greensand, near Bon church, Isle of Wight. An earthy nodule, containing 38-15 per cent, of metallic iron. 2835. Clay iron ore dredged up off the coast of the Isle of Wight and sent to Cardiff where it was sold for 10s. a ton, and used in considerable quantity at the Ebbw Yale Iron Works. It is a nodule from the ironstone beds of the Lower Greensand series. 2836. A black oolitic iron ore from Ireland. Examined by Dr. Percy for Mr. Blackwcll. Locality unknown. 2837. Carbonaceous ironstone called " Brass " from the Park Pits, South Wales. Contains 27-88 per cent, of metallic iron and is coarse grained and black. 2838. ft Brass " iron ore, occurring in the coal at Blaenavon, South Wales. 2839. " Coal Brass " iron ore from the Ocean Steam Com- pany's Pits, Ystradd, Pont-y-pridd, South Wales. Analysed by E. Smith. Ferrous carbonate Magnesium carbonate - Calcium carbonate Manganous carbonate - Coal - Ferric oxide Silica - - '--; Alumina Phosphoric acid Ferrous sulphide Water - 99-36 Equivalent to 31-78 per cent, of metallic iron. 2840. Gossan iron ore containing tin. From Holme Chase, Ashburton, Devonshire. Communicated by Geo. Malcolm. A brown irregular mass, accompanied, by a button of tin which has been melted out of a portion of it. FOREIGN IRON ORES. Ores from France. 2841. Ironstone from Niedepas, Ariege, France. An alternation of bands of siliceous and ferruginous matter which have been squeezed together. Apparently not rich in iron. U 61955. 1 322 2842. Mammillated brown haematite from Ariege, France. Massive within and with radiating nearly black crystals on the surface. 2843. Brown haematite from Ariege, France. , This shows radiate crystallisation in various parts of its mass, mixed with earthy parts and is remarkably smooth on one surface. 2844. Iron ores from Cherbourg. These are micaceous haematite of greater or less purity. There are four samples, the most micaceous from 11 metres below the surface. Second. 15 metres below the surface. Third, more massive from La Roche Dion, and fourth, earthy looking and compact ' from La Roche Dion. Analysed by W. J. Ward, 1866. Iron ores from Holland. 2845. Bog iron ore from old lake deposits in Holland. A brown concretionary limoriite of quaternary age. Communicated by J. E. de Fry, 2846. .Bog iron ore from Holland. A more completely solidified mass of the same kind. Communicated by Mr. Bleekrode. Jron ores from Germany. 2847. Spathic iron ore from Siegen, Rhine Provinces. A massive ferrous carbonate occurring in a vertical wedge-shaped vein in the Coblentz slates of the Lower Devonian period. See Phillips' Ores and Ore Deposits, p. 272. 2848. The same spathic iron ore from Siegen after calcination. 2849. Variety of spathic iron ore from Siegen, containing some copper pyrites. See Phillips' loc. at p.-273. 2850. Iron ore from Westphalia. It consists of a deposit of quartz sand, consolidated by ferric oxide on the surface but lying loose in the interior. 2851. Iron ore from Westphalia. A ferruginous grit. Communicated by Mr. Ormsby. 2852. Clay iron ore from Westphalia. Communicated by Mr. Ormsby. Appears to be part of a nodule. 323 2853. Bog iron ore from Olfen, Westphalia, Used largely in Prussia. A dark concretionary mass of dark brown limonite in small globules, similar to that formed in the Old Lakes of Holland. 2854. Red haematite from the North of Germany. Possibly from Elburgerodein the Harz where red haematite is worked, -contains 67*25 per cent, of metallic iron. Analysed by R. Smith. 2855. Spathic and brown iron ore from Germany. Possibly from the Siegen district. Consists of a vein of fine ferrous carbonate bounded by slate infiltrated by ferric oxide. 2856. Oolitic iron ore from 12 miles south of Hanover. This is probably from the neighbourhood of Salsgitter, where such oolitic iron ore, which is of the age of the Tealby iron ore, i.e. Neocomian, which it much resembles, is worked. Communicated by Mr. Hedley. 2857. Another example of the same oolitic iron ore. This is very much redder, especially in the matrix, which is not brown but red. Communicated by Mr. Hedley. Iron ores from Spain. 2858. Specular iron ore from Marbella, Spain. A black foliated mass of micaceous iron ore with a reddish dust. 2859. Micaceous iron ore from Marbella, Spain. A very line grained black foliated mass. Smelted at Dowlais Iron Works, 1870. 2860. Iron ore from Carthagena, Spain. A concentrically banded black concretionary mass, passing to a red colour on the surface. Smelted at Dowlais Iron Works, 1870. 2861. Brown iron ore from Spain. A black and brown concretionary mass of limonite, containing 53 33 per cent, of metallic iron, Communicated by J. Joule, 1873. 2862. Iron ore from Santander, north-west of Spain. A red earthy haematite, partly changed to limonite and bound by irregular bands of black oxide. Smelted at Dowlais, 1870. 2863. Altered spathic iron ore from Garucha, Spain. A solid mass with hollow spaces lined with crystals. These have the rhombohedral form of ferrous carbonate, but are mostly decomposed to a brown oxide, i.e., they are pseudomorphs of limonite after chalybite. 2864. Spathic iron ore from Bilbao, Spain. This is a crystalline mass, with faces arranged nearly parallel to those of a rhornbohedron, but it is black externally and red dust internally, X 2 324 so that it is a decomposed chalybite, mostly now haematite. It contains 15-58 per cent, of metallic iron. 2865. Micaceous hsematite from Bilbao, Spain. Smelted at Dowlais. A solid mass composed of irregular haematite crystals with red powder on the surface, 2866. Specimen illustrating the conversion of iron pyrites into brown iron ore. From Santander, Spain. Communicated by Mr. Bauerman, 1873. No. 1 is a mass of pyrites, partially converted into brown haematite, but still showing its original nature. No. 2 shows the cubical crystals of pyrites in its drusy cavities, but they are entirely converted into brown hgeinatite. No. 3 is a massive piece, with a few druses entirely altered into haematite. No. 4 is a stalactitic vacuous mass obviously formed by the evaporation of water containing a salt of iron solution. 2867. Limonite from Ribetto, San Pedro. A brown, banded, earthy deposit, of obviously modern formation. Iron ores from Portugal. 2868. Massive brown hsematite from Mongas, near Lisbon. Analysed by W. J. Ward, 1867. Communicated by Mr. Oakes. Contains 82 '48 per cent, of ferric oxide. The remainder is 5 '91 clay and sand, 8*20 loss on calcination. There is a trace of phosphorus and 0- lo per cent, of sulphur. This is equivalent to 57 '74 per cent, of metallic iron. ' 2869. Second specimen of hsematite from Mongas, near Lisbon. The two were averaged by the above analysis. 2870. Iron ore from Portugal. Smelted at the Dowlais Iron Works, 1870. A semi-micaceous, partially vacuous mass of black colour, weathering brown. Iron ores from Sweden and Norway. 2871. Micaceous iron ore from the Jarna Mines, Sweden. A compact crystalline black mass of ferric oxide. 2872. Micaceous iron ore from the Torola Mines, Sweden. A similar compact crystalline mass. 2873. Micaceous iron ore from Fetters Mine, Thorsaker, Sweden. A fine grained black crystalline rock with feeble signs of foliation. 2874. Micaceous iron ore from the Ys Mine, Thorsaker, Sweden. A very fine grained, somewhat foliated mass of black crystals. 325 2875. Iron ore from the Stenebo Mines, Sweden. An excessively fine grained, foliated and banded rock. This is the only ore of the above five which cannot be smelted by the simple addition of a suitable quantity of lime, but requires 50 per cent, of slag. All of these were communicated by C. Eckinan in 1848. They occur as portion of the crystalline schists of the Archasan epoch. 2876. Micaceous iron ore from Sweden, locality unknown. It contains 60'37 per cent, of metallic iron, has an insoluble residue of 14*07, and contains traces of phosphorus and sulphur. 2877. Coarse micaceous iron ore from Langban, Wermland, Sweden. 2878. Fine micaceous iron ore from Langban, Wermland, Sweden. A very massive compact rock of black colour. 2879. Rock from the Petersberg Mines, Wermland, Sweden. This is a basic crystalline rock, and does not resemble an ordinary haematite or other iron ore. It is probably a piece of the "country rock." 2880. Iron ore from the " Stor " Mine, Petersberg, Wermland, Sweden. This is a massive black ore with a drusy cavity, in which are developed octahedral crystals of magnetite. 2881. Iron ore from Langban Mines, Wermland, Sweden. A fine grained micaceous hematite, with some scattered crystals. 2882. Iron ore from the Stor Mine, Petersberg, Wermland, Sweden. A massive magnetite with portion of a drusy cavity, showing the mineral in rhombic dodecahedral and trapezohedral crystals. 2883. Iron ore from the Kran Mine, Petersberg, Wermland, Sweden. Very massive and minutely crystalline. These ores of Wernland are all referred to the crystalline schists of Archaean age. 2884. Iron ore from Taberg Smaland, Sweden, after calcination. From the Swedish Department, International Exhibiticn, 1862. The samples have an exterior coating of red solid matter, and within are composed of small black crystals in a dull white matrix. The rock of Taberg is said to be a mixture of magnetite and olivine. See Phillips' Ores and Ore Deposits, p. 395. 326 2S85. A series of ores from the Mines of Garpenberg, Wermland, Sweden. Named after their localities. They are all fine micaceous ha3inatites y and are arranged in the order of their coarseness, the most compact being last, i, ICnutsboi Tolkerna; 2, Bispberg No. 2 ; 3, Orlirige i Nor- bergsfaita; 4, Rynshytte Sjagrufora; 5, Bispberg No. 1; 6, Holm ,- 7, Kynshutte Compagne ; 8, Langviken. 2886. Bog iron ore from the moors at Axe wallsbod a., Sweden. . A hydrated peroxide of iron of recent formation. 2887. Lake ore from Lund Lake, Sweden. A hydrated peroxide of iron formed in lakes of a less depth than 30 feet from ferruginous waters, derived from the decomposition of the neighbouring mass of crystalline haematite. It is said to be due to the agency of an infusorian. The ore when first collected is uniformly slimy, but on drying it hardens to lumps of various sizes. The present is called " Penny ore." 2888. Lake iron ore from Yxem Lake, Smaland, Sweden. This is of smaller size when dried, and is called " Beau ore." 2889. Lake iron ore from Yxem Lake, Smaland, Sweden. This hardens into the smallest sized lumps, and is consequently called " Peas ore." 2890. Lake iron ore from Axewallsboda Lake, Astrogathi,. Sweden. This consists of coarse, dark, irregular lumps, found near where the Bog iron ore, No. 2886, occurs. 2891. Iron ore from Gellivara Lulia, Lapponark, Sweden,, lat. 67 20'. A massive crystalline rock of coarse isodiametric crystals of mag- netite and felspar ? the former far the most abundant. 2892. Iron ore from Gellivara, Lapland. A schistose variety of the same ore as No. 2891, with very little felspar. It is said to be titaniferous. These belong to the crystalline schists, presumably of the Archa3an period. 2893. Piece of a quartz vein, from the Kron Mine, Peters- berg, Wermland, Sweden. Some of the quartz crystals are coloured black by the magnetite. 2894. Titaniferous iron ore from Egersund, Norway. Smelted at the Dowlais Iron Works, 1870. A massive, coarsely crystalline rock of bluish-grey colour, between bands of a green: silicate. 327 2895.. Lake iron ore from Norway. Consists of rounded pear-like bodies of dark brown limonite, showing a concentric structure within; contains 36-21 per cent, of metallic iron. Communicated by R. Nesbitt, 1866. Iron ores from other European countries. 2896. Micaceous iron ore from Elba. Smelted at the Dowlais Iron Works, 1870. This ore occurs in veins and beds. Of early geological date. 2897. Beach pebbles of haematite, collected on the shore afc Marina di Rio, Elba. 2898. Iron ores from Russia, locality not stated. They are brown earthy masses of concretionary limonite; (1) is called Zingary's ore, (2) is Karakuba ore, (3) the same (spelt Carracuba), (4) Dravidsky's brown ore. Communicated by the " New Russia Company," 1873. 2899. Magnetic iron ore sand from Turkey, locality not stated. It has been assayed by melting 5,000 grains with lime, china clay, &e. and 1,000 grains of anthracite, by which method it yielded a button weighing 3,470 grains. This is equivalent to a per-centage of 69 '4 of metal. Some of the grains have an Octahedral shape, and all are strongly attracted by the magnet. Iron ores from Africa. 2900. Natural lodestone frt>m the Cape of Good Hope. Massive fragments of magnetite of great magnetic strength. 2901. Iron ores from Algeria. Two are pieces of hematite, one is a concretionary limonite, the others are red and dark purple clays. See Phillips' Ores and Ore Deposits, p. 515. Iron ores from the East Indies. . 2902. Nodule of earthy brown limonite from Singapore. Communicated by Dr. Lockhart. Contains 46-64 per cent, of metallic iron. 2903. Iron ore sand from Bandai Salangore, Straits Settle- ments. Crystals and fragments of haematite, which are not attracted by the magnet, with sand grains intermixed. 2904. Massive black haematite in a nodule from near Sairi, the Punjaub, India. 328 Iron ores from China and Japan. 2905. Earthy brown concretionary massive haematite from Rung Chung, China. Communicated by J. Henderson. Analysed by R. Smith, 1875. 2906. Iron ore from Kai-Ping, China. A dark haematite schist. Communicated by W. Lawford. Analysed by W. J. Ward, 1879. 2907. Three small samples of iron ores from China, locality not stated. One is a brown concretionary ron ore containing 58 -4i per cent, of metallic iron ; the second is a magnetite containing 70-25 per cent, of metallic iron ; and the third is an earthy ochre, yielding a scarlet powder on calcination, and containing 43-20 per cent, of iron. Analysed by R. Smith, 1874. 2908. Mass of crystalline iron tf ore " from the neighbour- hood of Yeddo, Japan. This is in small crystals run together, and it cuts like a metal. It is said to be forged direct by the Japanese. Communicated by R. C. May, 1868. Iron ores from Australasia. 2909. Series of specimens illustrating the purifying of superficial iron ore by the Port Philip Company, New South Wales, Australia. The material is called " blanket sand." No. 1 is the quartz grains separated by levigation after grinding. No. 2 is the concentrated sand after extraction of the quartz. No. 3 is the same in fine powder, con- sisting of a mixture of grains of magnetite and of pyrites. No. 4 is the amount of magnetic iron ore attracted by the magnet and thus separated from the rest. No. 5 is the residue of pyrites which is left untouched by the magnet. Communicated by the Port Philip Company, 1862. 2910. Australian iron ore, locality not stated. A reddish grit, largely composed of crystals of magnetite. Communi- cated by Fowler & Co., 1874. 2911. Titaniferous iron ore from New Zealand. It has been fused with charcoal alone in a Cornish crucible. The surface of the melted mass is coated with long acicular crystals which often make their appearance when such ores are assayed in the dry way. Iron ores from Canada. 2912. Titaniferous iron ore from the Laurentian Rocks of Canada. It is a black schistose rock. Communicated by Mr. Bullen, 1874. 329 2913. Another example of titaniferous iron ore, not so crystalline as the last. Communicated by Mr. Bullen, 1874. 2914. Micaceous iron ore from Nova Scotia. The hematite is in very large lamellar crystals, standing across a vein in a red earthy rock. 2915. Slate used as iron ore from Nictaux, Anapolis Valley Nova Scotia. These are ordinary masses of Cambrian or Silurian fossiliferous slate, strongly impregnated with ferric oxide. 2916. Bedded haematite, McLennan's Mountain, Nova Scotia. A schistose rock, consisting almost entirely of haematite. Commu- nicated by Gr. M. Dawson, 1873, with the four following specimens. 2917. Limonite from East River, Pictou County, Nova Scotia A large fibrous mass in several layers of perpendicular crystals. 2918. Specular iron ore from East River, Pictou County, Nova Scotia. Irregular massive crystalline haematite. t 2919. Spathic iron ore from Sutherland River, Pictou County, Nova Scotia. An aggregation of small rhombohedral crystals. 2920. Bedded haematite, " Blanchard's," Pictou County, Nova Scotia. A compact foliated rock. 2921. Bog iron ore from St. Etienne, St. Maurice County Canada. Small irregular pieces of earthy limonite. 2922. Bog iron ore from St. Marguerite, St. Maurice County Canada. Irregular concretionary masses of dark and light brown limonite. , .Iron ores from America. 2923. Iron ore from the Suckasunny Mine, New Jersey .TJ.S.A. This is composed of a mass of fair sized black haematite crystals arranged uniformly. It is considered to be the best of the New Jersey ores. 330 2924. Iron ore from the Suckasunny Mine, New Jersey, U.S.A., containing phosphate of lime. The crystals in this are smaller, and they are interspersed with green- crystals of apatite. These ores form a part of the Archasan schists. 2925. Iron ore from Andover, New Jersey,. U.S. A. These are massive red bsematite, partly fibrous and partly in large crystals. 2926. Iron ore from Andover, New Jersey, U.S.A. This is a portion of a banded vein having quartz in the centre and surrounded by fibrous radiating haematite. 2927. Haematite from Marquette, Michigan, U.S.A. A black compressed foliated rock. The Marquette deposits have been separated from the Huronian as a distinct group. Communicated by the Jackson Iron Company. 2928. Clay iron ore from Virginia, U.S.A. A brown banded carbonaceous deposit, containing 32*8 per cent, of metallic iron. Analysed by W. J. Ward, 1875. 2929. Iron ore from Western Virginia, U.S.A. A tufaceous brown limonite, containing 48 '69 per cent, of metallic iron. Communicated by R. J. Carpenter. Analysed by R. Smith, 1873. 2930. Residue from the extraction of zinc from Frank- linite (T), smelted for iron at the New Jerse}^ Mining Company's Works, Newark. A scoriaceous black mass. Communicated by J. Bauerman, 1878. 2931. Franklinite roasted, from the Stirling Works, New Jersey, U.S.A. The residue, after the zinc has been extracted, used as an iron ore. 2932. Iron chloride from the Little Sliver Mine, Leadville, Colorado. A scoriaceous mass accompanying silver ores. 2933. Magnetic iron ore with iron pyrites: The Cornwall ore, Cornwall, Lebanon, Pennsylvania, U.S.A. Shows that even an ore which contains so much pyrites may, after roasting, be smelted with advantage. Communicated by H. Louis. 2934. Laminated form of Gothite, called Lepidokrokite, from a bed of the brown iron ore used at the Glyndon Furnaces, Eastern Pennsylvania. It is a hydrous oxide of iron, the layers of which are concretionary and have a mammillated and fibrous structure. See Dana's System of Mineralogy, p. 170. 331 2935. Native honeycomb iron ore, smelted at the Dunbar Iron Furnace, Pennsylvania. A complete analysis of this, which is an argillaceous ore, gives the following : Ferrous oxide - 45*634 Ferric oxide - - 2'057 Alumina - 3 '740 Lime- - - - - 0*014 Magnesia - - - 1*678 Silica - - 0*424 Carbonic acid - 29*745 Phosphoric acid - - 0*068 Iron bisulphide - 0*754 Combined water - - 0*042 Hygroscopic water at 100 C. 0*074 Organic matter - 1 * 324 Ignited insoluble residue - 15*568 101*122 The insoluble residue contains silica 10*844, alumina 4*240, lime '034, magnesia *439, and traces of ferric oxide. This is equivalent to 35*823 per cent, of metallic iron. Other analysis of the same ore for iron only have shown from 28 to 42 per cent. 2936. Native honeycomb iron ore calcined, smelted at the Dunbar Iron Furnace, Pennsylvania. This is now a red earthy mass, resembling haematite. 2937. Native Big Bottom iron ore, smelted at the Dunbar Iron Furnace, Pennsylvania. It is a homogeneous massive dark earthy rock, whose analysis shows : Ferrous oxide - 45*274 Feme oxide - - traces. Alumina - 3 445 Lime - - 1*456 Magnesia - - 1*464 Silica - - 0*195 Carbonic acid - - 30*322 Phosphoric acid - 0*170 Iron bisulphide - - traces. Combined water - - 0*029 Hygroscopic water at 100 C. - 0*003 Organic matter - * 947 Ignited insoluble residue - 16*700 100*005 The insoluble residue contains silica 1 1 * 046, alumina 4 697, ferric oxide 0'643, lime 0*264, magnesia 0*047. 332 2938. Native Big Bottom iron ore calcined, used at the Dunbar Iron Furnace, Pennsylvania. It is only externally changed to a red colour. 2939. Jackson iron ore from Lake Superior, smelted for Bessemer iron, at the Dunbar Furnace, Pennsylvania. A massive schistose silky red specular ore. 2940. Republic iron ore from Lake Superior, smelted for Bessemer iron at the Dunbar Furnace, Pennsylvania. A brilliant black micaceous ore. It contains 69 '88 per cent, of ferric oxide and O'Ol per cent, of phosphorus. 2941. Champion iron ore from Lake Superior, smelted for Bessemer iron at the Dunbar Furnance, Pennsylvania. A brilliant black micaceous ore of fine grain. Analysed by Britfcon gives : Metallic iron - Oxygen with iron Sulphur Phosphorus Lime - Moisture Insoluble matter 99-83 Of the 69 '92 per cent, of iron 22 '97 is combined in the ferrous, 46 '95 in the ferric state. 2942. Washington iron ore from Lake Superior, smelted for Bessemer iron at the Dunbar Furnace, Pennsylvania. A. very fine micaceous ore, said to be magnetic. Analysed by Britten gives : Metallic iron - - 68 46 Oxygen with iron - - 27 '22 Phosphorus - O'Ol Lime - 0'14 Moisture - 1 1 9 Insoluble matter - - 2 60 99-62 Of the 68*46 per cent, of iron 19 '30 is combined in the ferrous, 49 -16, in the ferric state. 2943. Iron Mountain magnetic iron ore, smelted at the Dunbar Furnace, Pennsylvania. Coarse irregularly crystallised and black, containing on the average 60 '68 per cent, of metallic iron. 333 2944. Chaffey iron ore, smelted at the Dunbar.Iron Furnace, Pennsylvania. Coarse, black and crystalline, having the following composition : Magnetic oxide - - - 60-57 Ferrous oxide - - - 10-03 Alumina - 3-69 Lime ----- 0-61 Magnesia - - - 4-96 Silica - - 7-08 Phosphoric acid - - - trace Sulphur - 0-82 Titanic acid - - - 11-43 99-19 This is equivalent to 52 36 per cent, of metallic iron. 2945. "Mill cinder" used as an ore for smelting at the Dunbar Iron Furnaces, Pennsylvania. It is a black scoriaceous refinery slag, from the mills. 2946. Lodestone or magnetic iron ore from Brazil. 2947. Micaceous iron ore from Itabira, Minas Geraes, Brazil. A schistose rock almost entirely composed of haamatite spangles. 2948. Concretionary iron ore from Para, Brazil. A sandstone infiltrated with hydrated ferric oxide. IRON ORES FROM UNKNOWN LOCALITIES. 2949. Crystalline magnetic iron ore. Analysed by C. Tookey. Contains 38 per cent of metallic iron, and 1-31 per cent, of sulphur. Communicated by Mr. Appleton. 2950. Massive earthy brown haematite. Communicated by Mr. Taylor. 2951. Oolitic iron ore. A brown haematite, containing 28-02 per cent, of metallic iron. Communicated by the Earl of Ilchester. It looks like the Westburj ore. 2952. Fibrous black haematite, developed on a massive piece and showing a stalactitic development of haematite on the smooth surface. 2953. Black oolitic iron ore. Analysed by Dr. Percy for Mr. Blackwell. Is it Welsh pisolite ? 334 2954. Compact Ilmenite. Titaniferous iron ore. Communicated by Mr. Burchell, with two tubes of materials derived 'from it. 2955. Magnetic iron ore. Communicated by Mr. Arundel, 1870. Analysed by C. Tookey. Ferrous oxide - Ferric oxide Manganous oxide Alumina Lime - Magnesia Phosphoric ncid Sulphur Water - Organic matter Insoluble residue 99-75 Equivalent to 42 per cent, of metallic iron. 2956. Spathose iron ore with a border of pyrites. 2957. Specimen resembling spathic iron ore, but containing only 6 ' 1 1 per cent, of metallic iron. Analysed by R. Smith. FALSE IRON OSES. 2958. Oxide of iron conglomerate. From Toddington Manor, D unstable, Kent. It forms a thin bed about three feet from the surface and consists of siliceous pebbles im- bedded in a matrix of limonite. As analysed by R. Smith, it contains 20-42 per cent, of metallic iron. Communicated by Major C. Cooper. 2959. Supposed iron ore from the New Forest, Hampshire. Two specimens derived from the Upper Eocene series. One is a compact sandstone impregnated with brown haematite. The other is a slaggy mass containing abundant fragments of charcoal, probably an attempt at smelting. The metallic iron obtainable from the sandstone amounts to 16-24 per cent. 2960. " Iron ore " from Providence, Ashton Court, Bristol. An analysis of this has been given as silica 22-25, oxygen 23-20, and iron 54 55, but this has been found by J. Spiller to be erroneous. 2961. Mass of red clay, locality unknown, sent as a sample of iron ore. On examination it is found to contain only 3J per cent, of metallic iron. 2962. Specimen sent as spathic iron ore from East Tarbert, Lochfyne, Argyleshire. It consists essentially of carbonate of lime and contains only 1J per cent, of metallic iron. 335 2963. Limestone sent as spathic iron ore from Bonnsville Court, Saundersfoot, Pembrokeshire. It contains only 1 52 per cent, of metallic iron. 2964. So called " argillaceous iron ore " from the Lias. From near Middlesborough. It consists of a bed of clay showing one in cone structure with a certain small amount of iron. 2965. Cement-stone nodule containing iron and mistaken for an ironstone. It is used for making Roman cement of the best quality and is called the screw or bastard stone, near Darlaston. Communicated by Mr. Clift. 2966. Material from Tioga, New York, said to have wonderful powers in the manufacture of steel, &c. It is nothing but some red micaceous shale of no value whatever. THE PRODUCTION OF PIG IRON. MATERIALS USED AS FLUXES. 2967. Limestone used in the blast furnace at Finspong, Ostgothland, Sweden, with the Swedish iron ores. A white crystalline limestone. Compare Percy's Metallurgy, Iron and Steel, p. 553. 2968. Limestone used as a flux in the Allentoun Furnace, on the Lehigh Kiver, Eastern Pennsylvania. A black compact marble. 2969. Limestone used at Newland Furnaces, Ulverstone. Grey compact Carboniferous Limestone of Lancashire. 2970. Limestone used at Ystalyfera, South Wales. The dark grey Carboniferous Limestone of South Wales. 2971. " Coal limestone " used as a flux in smelting iron at the Dunbar Iron Furnaces, Pennsylvania. Analysed by -Habershaw. Gives Calcium carbonate - 86-58 Magnesium carbonate - - 3-71 Ferric oxide and alumina - 6-25 Silica - - 0-76 Organic matter - 0-21 Insoluble- - 2-83 100-34 336 2972. "Mountain limestone" used as a flux in smelting iron at the Dunbar Iron Furnaces, Pennsylvania. Analysed by Maynard and Van Rensselaer. Gives Calcium carbonate Magnesium carbonate - Ferric oxide and alumina Insoluble 99-04 r SLAGS PRODUCED IN THE MANUFACTURE OF PIG IRON. Non-crystalline slags. 2973. Slag from Gartsherrie blast furnaces. It is produced in a hot-blast furnace, manufacturing the best quality (No. 1) of pig iron. It is compact internally, and has a coat of grey glass. 2974. Blast furnace slag; from a hot-blast furnace, making good rail iron at the Cyfartha Works, South Wales. Communicated by D. Wilson, 1871. A black glass, with narrow bands of white, which are bent round into a fold, and drawn out by the motion of the molten mass, after the manner of a lava current. 2975. Blast furnace slag from Bromford Iron Works. An olive green, glassy mass, but with bands and scattered individuals of lighter tinted tetragonal prisms. 2976. Blast furnace slag from the Ystalyfera Iron Works, South Wales. Produced with anthracite as fuel ; a brown earthy-looking mass, which becomes a black glass at the surface, where it contains isolated light coloured tetragonal prisms. 2977. Blast furnace s-lag, produced from spathic ores at the Ebbw Vale Iron Works, South Wales. Communicated by GL Parry, 1859. Green glassy masses of two distinct tints, light and dark, sharply marked off from each other, and both with abundant contorted now lines. 2978. Black slag, produced when a furnace (locality un- known) was deranged. The derangement was due to some interruption in the descent of the material in the blast furnace, as observed at the top, and its subsequent dropping suddenly on the twyers, as seen by the sudden fall of the surface. It is a black compact mass, with a brilliant black glassy surface. The iron made was white iron. 2979. Slag from a London iron foundry. Communicated by J. C. Crosson, 1876. A scoriaceous mass with smooth undulating glassy surfaces. 337 2980. Scoriaceous, semi-crystalline, dark-grey slag, produced from one-third Eston, and two-thirds Weardale, iron ore. 7| cwt. of Weardale and Eston ores were smelted with 4 cwt. of coke, and 2 J cwt. of limestone. 2981. Iron slag, containing titanic acid. No. 1. A black, semi-crystalline, scoriaceous mass; locality not stated. Compare Percy's Metallurgy, Iron and Steel, p. 507. 2982. Iron slag with titanic acid. No. 2. A thin sheet, slightly scoriaceous in the centre, but becoming com- pact and grey, and at the edges more glassy and blue. Compare Percy's Metallurgy, Fuels, 1875, p. 56. 2983. Iron slag with titanic acid. No. 3. Dark and semi- vitreous. 2984. Lavender-coloured blast-furnace slag, from Russell Hall's furnaces, near Dudley. The slag is compact, and the lavender colour is interspersed with green, and is spotted over with minute black specks or hollows. 2985. Pink-coloured blast-furnace slag from Ebbw Yale Iron Works. Communicated by Mr. Parry, 1859. It is uniformly coloured, and very finely scoriaceous, and light like a pumice. Said to be produced when the charge has contained much spathic ore. See Percy's Metal- lurgy, Iron and Steel, p. 506. 2986. Pink-coloured iron slags found on the road near Pontypool Iron Furnaces, South Wales. (Three specimens.) Two of these are scoriaceous, with large vesicles, and on breaking them across to obtain a fresh surface, it is seen that the pink colour is merely superficial, and that the slag is green within. The second specimen shows a green compact interior and a coating of pink ; the third is more glassy, and is bluish in the interior. It appears, there- fore, that the pink colour is the result of superficial alteration or weathering. 2987. Pink-coloured slag from the Dowlais Iron Works, South Wales. Communicated by E. Biley. These are fragments of glassy slags which once were blue, but now shade through green to pink on the surface. ' The colour may depend on the presence of manganese in the 2988. Pink-coloured blast-furnace slag from the Glengarnock Iron Works, 1885. A scoriaceous mass, probably weathered to the centre. U 61955. v 338 2989. Blast-furnace slag produced when making No. 1 iron, (No. 3179 of this catalogue), at the Newland Furnaces, Ulvers- tooe, 1856. A dark purplish translucent glass with feeble signs of the flow of the molten material. This and the five following were communicated by Mr. Roper. 2990. Blast-furnace slag produced when making No. 3 iron at the Newland Furnaces, Ulverstone. A bluish, translucent, solid glass with a slight tinge of green on the surface. 2991. Blast-furnace slag produced when making No. 2 iron at the Newland Furnaces, Ulverstone. Two specimens, one is a compact bright blue non-translucent mass, with fine pin holes, and a darker blue more glassy margin. The other is a cindery mass from the surface, with some unaltered scales of hematite imbedded. It is a transparent glass with floating blue particles of brilliant tint. Compare Percy's Metallurgy, Fuels, 1875, on the blue colour of slags. 2992. Blast-furnace slag produced when making No. 5 iron_ at the Newland Furnaces, Ulverstone. A black vitreous froth, with large and small cavities, excessively light. 2993. Blast-furnace slag produced when making No. 6 iron at the Newland Furnaces, Ulverstone. A light scoriaceous black mass, most glassy and with the largest cavities on the outside portions, one of which contain bits of charcoal, &c. Produced in the refinery ? 2994. Blast-furnace slag produced in making No. 6 iron at the Newland Furnaces, Ulverstone. A greenish black opaque glass with a scoriaceous surface. 2995. Slag from No. 6 iron at the Newland Furnaces, Ulverstone. A solid heavy regulus-like mass with a glassy surface with imbedded gravel, The iron made was unsaleable. See No. 3183. 2996. Black glassy slag in small irregular fragments. Communicated by Mr. Dalton. 2997. Blast-furnace slag from the Cyfartha Iron Works, South Wales. A very uniform clear brown glass. 2998. Blast-furnace slag from the Cyfartha Iron Works, 1889.. An opaque grey stone changing towards the surface, through a blue tint to a dark glassy banded layer. 339 2999. Blast-furnace slag from the furnace casting in 1851, at a time that three qualities of iron were obtained. Scoriaceous below, green, compact in the centre, dark green and glassy on the top. 3000. Blast-furnace slag showing an iridescent surface. A thin greenish opaque glass with a broad smooth surface, locality unknown, two specimens. 3001. Blast-furnace slag with iridescent particles on its surface. A piece cf green opaque slag probably from the same furnaces as the last, partly glassy and partly crystalline. The iridescence is confined to the glassy portion and dies away as it passes with the crystalline. 3002. Uniform black glassy blast-furnace slag, produced in smelting Ashton iron ore at Dowlais, South Wales. Communicated by E. Riley. 3003. Vesicular slag from the blast-furnaces at Russell Hall's Iron Works, Dudley, 1861. A honeycombed brown-coloured mass, presumed to be formed by the occlusion of air by the molten slag which separates but cannot escape on the solidification. See Percy's Metallurgy, Fuels, 1875, p. 55. 3004. Vesicular green slag from the blast-furnaces at the Newlaud Iron Works, Ulverstone. The cavities are almost always separated by some thickness of the green semi-vitreous slag. The green colour is said to be due to the presence of manganous oxide. Communicated by E. Riley. 3005. Pumice-like blast-furnace slag from the Blaina Iron Works, South Wales. It is perfectly white and contains larger and smaller holes. It is called " Furnace pumice " and is produced by the slag coming in contact with water while in a molten state by which means steam is generated in its midst. See Percy's Metallurgy, Iron and Steel, p. 516. 3006. Blast-furnace slag showing a columnar structure. Communicated by J. Blair, 1886. This was produced many years ago at the Wingerworth Iron Works, Chesterfield, in smelting oolitic ores, but the details of the circumstances are not on record except that the furnace was " gobbed " at the time. The analysis gives Silica - - 29-70 Alumina - - 22-00 Lime - - 46-53 Manganous oxide - trace Magnesia - 1-50 99-73 Y 2 340 The column is pentagonal, with concave sides, and the whole has a semi- vesicular lava-like texture. 3007. Blast-furnace slags from smelting manganese ores to make spiegeleisen. From the furnaces of Sir J. Brown & Co., Sheffield. Some of these are of an olive green opaque glass, one is coated with a layer of dark brown transparent glass, one is more or less compactly crystalline, and one has drusy cavities in which are long prismatic needles resembling ferro-manganese. 3008. Slag from off the surface of the molten iron in smelting Ashton iron ore. This ore contains barytes. It was smelted at Dowlais Iron Works, and this material ran out on the top of the pig and must have lain between the ordinary cinder and the molten pig. It contains sulphides. Communicated by E. Biley. It has been analysed by R. Smith and found to contain 69*10 of sulphide of iron, 20-28 of barium sulphide, and small quantities of calcium, magnesium, potassium, sodium and manganese, and 08 of copper. See Percy's Metallurgy, Iron and Steel, p. 895. 3009. Blast-furnace slag from the ironworks of Seend, Wiltshire. They smelt oolitic ore here. It is a bluish green opaque glass with scattered black spots of semi-crystalline slag. Communicated by H. Bauerman, 1875. 3010. Slag which collects in the Cowper hot-blast stoves, when the furnaces are making spiegeleisen. At Sir J. Brown & Co.'s Iron Works, Sheffield. Communicated by J- Blair. The ore used was Spanish. It is an opaque brown glass and has been analysed by W. Galbraith and shown to contain Zinc oxide - Ferrous oxide - Manganous oxide Alumina Potash Soda - - - - Silica - 99-93 Associated with it was some zinc dust containing 2-23 per cent, of potash and 1-20 per cent, of soda. 3011. Slag from No. 3 blast furnace at Ebbw Yale when making spiegeleisen. The spiegeleisen produced contained about 16 per cent, of manganese. This slag is green, semi-crystalline, and compact. It contains a number of crystals in the form of tetragonal prisms. They are lighter in 341 tint and have cracks along the diagonals, with a hollow in the centre, like the crystals of chiastolite. Communicated by Gr. Fitz-Brown. Foreign Slags. 3012. Blast-furnace slag produced in making Bessemer pig iron at the Royal "Marienhiitte" Iron Works, Germany. Communicated by Gr. F. Becker. These are produced when the furnace is working well and smelting a mixture composed of 65 per cent, of spathic iron ore, 25 per cent, of manganiferous heematite, and 10 per cent, of siliceous haematite. The slag is allowed to cool slowly in large iron boxes, in which cavities are formed lined with a pink, often crystalline coating, the main mass having a green tinge. 3013. Foundry-furnace-slag produced at the Royal " Marienhiitte " Iron Works. Communicated by Gr. F. Becker. This is a product of smelting 25 per cent, of minette (i.e., Luxemburg oolitic ore), 25 per cent, of bog iron ore, 30 per cent, of calcareous haematite, and 20 per cent, of sphaero- siderite. These are of the same colours as the Bessemer slag, but more compact and less crystalline. 3014. Highly porous grey slag from the iron furnaces of Holland. Definite locality not given. It is almost like pumice, with a glassy surface, and is produced in the smelting of the ore No. 2845. Com- municated by J. E. de Fry. 3015. Blast-furnace slag from the iron furnaces called " Herzog-auguste Hutte," Dilienburg, Nassau. A glassy mass, with a stony under surface, with pieces of charcoal showing the nature of the fuel employed. The surface is marked by the flow of the semi-liquid mass. 3016. Blast-furnace slag from the " Herzog-auguste Hutte " furnaces, Dilienburg. It is a banded black glass, with scattered rectangular prisms of a grey colour. 3017. Another basic slag similar to the last, but without label. 3018. Blast-furnace iron-slag from the United States Black on one side, where it is scoriaceous ; yellowish grey on the other, where it is confusedly crystalline. 3019. Blast-furnace slag from Allentoun furnace. A solid, grey, stony mass, with rectangular prisms in parts of the surfaces ; lustre of the faces dull. 342 3020. Blast-fnrnace slag, locality uncertain. It consists oP a brilliant black glass, in which are embedded isolated grey spherulites with radiate crystallisation so coarse that sections look like corals. 3021. Bkst-furnace slag from smelting ores containing titanium at Espedal, Norway. Communicated by D. Forbes. A porous, semi-crystalline, stony mass, of brownish tint ; rapidly becomes quite compact, but has a black glass on the surface. 3022. Slag from a blast-furnace using charcoal as fuel, in Poland. A completely vitreous, coarsely vesicular, black mass. Analysed by W. J. Ward. It contains 7 *56 per cent, of ferrous oxide, 29-58 per cent, of aluminia, 52-67 per cent, of silica, 4-52 per cent, of lime, and 1 *27 per cent, of manganous oxide. This is equivalent to a loss of 5 88 per cent, of metallic iron. 3023. Slag from tbe blast-furnaces of the Northern Iron Company, Marquette, Michigan, U.S.A. A homogenous, black, slightly translucent glass. 3024. Banded slag from the blast furnaces of the Northern Iron Company, Marquette, Michigan. Black below and white above, with flow lines of the latter colour dying out in the former, the whole glassy. 3025. Pumiceous slags from the blast-furnace of tbe Northern Iron Company, Marquette, Michigan. One side is perfectly glassy and black, but it rapidly changes into a white pumiceous mass, where it has been brought into contact with water. 3026. Blast-furnace slag from the Wyandotte furnaces, Detroit. A black, slightly mottled, homogeneous glass, quite translucent. 3027. Blast-furnace cinder from Sweden. A light greenish opaque glass, with aggregations of black semi- crystalline slag. 3028. Slag from a Swedish iron blast-furnace. From the International Exhibition, 1862. It is greenish grey, compact, and spherulitically crystallice within, and suddenly changes with an irregular boundary to a translucent green glass on the surface. It has flowed over cinders. 3029. Blast-furnace slag from the ironworks of Finspong, Sweden. Communicated by C. Eckman. A leak-green, opaque, vitreous mass, spotted with black, and darker green on the surface. The charge which 343 is used in these furnaces, which are employed in the manufacture of iron for cannon, is given in Percy's Metallurgy, Iron and Steel, p. 553, by which it appears that the ores used are very manganiferous, hence the green colour. 3030. Iron-slag from the Province of Borgarfjordr. in Ice- land. Communicated by Dr. Hjaltelin, of Reykjavik. Found near the Surturbrands beds, which are of Miocene age. It is made from a very ferruginous basalt, which till recently has been worked in Germany for iron. It is a black mass of superimposed flows of molten matter, with large cavities, and of compact substance. 3031. Slag from a furnace making spiegeleisen at Mulheim, on the Rhine. Communicated by H. Bauerman. The slag is made with 50 per cent. of limestone in the charge, and has disintegrated spontaneously on cooling. 3032. Slag from working No. 2 iron at the New Jersey Zinc Works.. Newark, U.S.A. As this has the colour of spiegeleisen slag, and as spiegeleisen is produced at these works, this appears to be the slag of the same. It is a dark brown glass, touched with green. 3033. Slag from the spiegeleisen-furnace of the New Jersey Mining Company, Newark, New Jersey, U.S.A. Communicated by J. Bauerman, 1871. An opaque, green glass, becoming crystalline in parts. Crystalline Slags. 3034. Basic slag from a hot-blast-furnace working with coke, near Dudley, South Staffordshire. This is the No. 1 of the Report on Crystalline Slags presented by Dr. Percy to the British Association in 1846, and the No, 2 of the "Slags of the Formula R 2 3 SiO 3 -f 2 (3 RO SiO 3 ) " of his Metallurgy, Iron and Steel, p. 497. It consists of transparent, square, tabular crystals, which have the following composition. Analysis by Dr. Percy. Silica .... Alumina Lime - Magnesia Manganous oxide Ferrous oxide Potash Calcium sulphide 99-81 344 3035. Basic slag from a hot -blast-furnace working with coke, near Dudley, South Staffordshire. This is No. 2 of the Report, and No. 3 of Percy's Metallurgy, Iron and Steel, p. 497. It consists of similar transparent tabular prisms, and has the following composition. Analysis by Dr. Percy. Silica Alumina - Lime - - - - Magnesia - Manganous oxide - Ferrous oxide Potash Calcium sulphide 99-26 3036. Basic slag from a hot-blast-furnace, Russell Hall. This is No. 3 of the Report above referred to, and No. 4 of Percy's Metallurgy, Iron and Steel, p. 497. The specimens show highly crystalline, black, square tables in drusy cavities, some of which have the angles truncated as described. These slags are said to have the following composition. Analysis by Dr. Percy. Silica - - - 37-63 Alumina - 12-78 Lime - - 33-46 Magnesia - 6-64 Manganous oxide - 2 64 Ferrous oxide 3-91 Potash - - 1-92 Calcium sulphide - 0-68 99-66 3037. Basic slag from Messrs. Blackwell's-hot-blast furnaces, working with coke. Russell Hall's Iron Works, Dudley, South Staffordshire. This is No. 4 of the Report above referred to, and No. 5 of Dr. Percy's Metallurgy, Iron and Steel, p. 497. It consists of a compact crystalline mass, snowing opaque, greenish prismatic crystals on the surface. These are not transparent, but show clear signs of being complex growths. It is possible that this (though labelled with a figure) may be wrongly identified. The analysis given, made by D. Forbes, is Silica - - 37-91 Alumina - - - 13-01 Lime - - - 31-43 Magnesia - - 7-24 Manganous oxide - - 2-79 Ferrous oxide - - - 0-93 345 Potash - 2-60 Calcium sulphide - - 3-65 99-56 3038. Basic crystalline slag, very similar to the last. This is unlabelled. It is more crystalline, the centres of the crystals being often transparent. With this exception the whole is well shown to be composed of complex crystals, some of which show with perfect clearness the black cross characteristic of chiastolite. 3039. Cold-blast-furnace slag from Phillip Williams' Iron Works, Wednesbury Oak, Tip ton, Staffordshire. This is No. 5 of Dr. Percy's British Association Report, and No. 1 of his Metallurgy, Iron and Steel, p. 497. This is very crystalline on the surface, the crystals being prismatic plates, overlapping and united. The analysis by D. Forbes gives Silica - - 39-52 Alumina - - - J5-11 Lime ----- 32-52 Magnesia - - 3-49 Manganous oxide - 2-89 Ferrous oxide - - - -2-02 Potash - - - 1-06 Calcium sulphide - - - 2-15 98-76 3040. Glassy variety of the same slag as the last, showing the isolation of the crystals in the glass. 3041. Blast-furnace slag from a hot-blast-furnace working with coke, from La Providence Iron Works, Marchienne Charleroi, Belgium. Communicated by S. H. Blackwell. This is No. 6, both in the Eeport above referred to and in Percy's Metallurgy, Iron and Steel, p. 497. It is dark brown, vacuous, half glassy, half crystalline j the crystals are indeterminable. The analysis by Dr. Percy gives Silica - - - - 42-06 Alumina - 13-05 Lime - - - 32-53 Magnesia - 1-06 Manganous oxide - 2-26 Ferrous oxide - - 4-94 Potash - - 2-69 Calcium sulphide - 1-03 Phosphoric acid - 0-19 99-81 346 3042. Intermediate blast-furnace slag from the Russell Hall's Furnaces, near Dudley, South Staffordshire. It is very tough, and consists of an agglomeration of small radiating crystalline masses, of a light yellowish brown colour. Analysed by A. Dick, giving Silica - - - - 47-08 Alumina - 12-91 Lime - - - 29-92 Magnesia - 4-79 ferrous oxide - - 1-00 Manganous oxide - 2-20 Potash 87 Calcium sulphide - 1-78 Phosphoric acid - 0-05 100-60 From this it is deduced that the formula of the crystals is " R 2 O 3 , Si O 3 + 3 (CaO SiO 3 )." 3043. Intermediate slag from the hot-blast-furnaees of L'Espe'rance, Seraing, Belgium. Communicated by S. H. Blackwell. This is No. 11 in Dr. Percy's Report to the British Association, 184(S, on Crystalline Slags. It is a brown vacuous mass, with confused interlacing crystals. Analysed by D. Forbes, and gives Silica - - - 55-77 Alumina - 13-90 Lime - - 22-22 Magnesia - - - -2-10 Manganous oxide * 2-52 Ferrous oxide - 2-12 Potash - - - 1-78 100-41 This approximates it to the formula, A1 2 O 3 Si O 2 -f 4 Ca O 3 Si 2 . See Percy's Metallurgy, Iron and Steel, p. 501. 3044. Blast-furnace slag, approximating to Gehlenite in composition, from the hot blast furnace of Oldbury, near Bir- mingham. It is mixed with pieces of coke and iron, and consists of three square crystalline tables of a white and transparent colour, with particles of sulphur here and there on their surface. This is No. 7 of the Report above referred to. Analysed by Dr. Percy it gave Silica - - 28-32 Alumina - - - 24-24 Lime - - 40-12 Magnesia - 2-79 Manganous oxide - 0-07 Ferrous oxide - - - 0-27 347 Potash - 0-64 Calcium sulphate - 0-26 Calcium sulphide - 3-38 100-09 This approximates it to the formula "3 Al 2 O 3 Si O 3 + 3(3 CaO, SiO 3 )." (t is the original specimen of artificial Gehlenite referred to in Dana's System of Mineralogy. See Percy's Metallurgy, Iron and Steel, p. 502. 3045. Crystalline slag, locality unknown. A blue glassy mass below, with greenish-grey, semi-opaque crystals, like those of No. 3037, forming a surface layer. They are square prisms, with pyramidal ends, standing perpendicularly to the surface of the slag, 3046. Coarsely crystalline surface of a slag, locality unknown. Below, this is composed of similar crystals to those of the last, but here the surface is covered with a dark coating, and shows crystals f in. in diameter of opaque greenish substance within, and of an octagonal prismatic shape with convex sides and complex in growth. 3047. Crystalline surface of a slag, showing an ingrowth of greenish opaque material from the four sides of a tetragonal prism having a dark centre as in chiastolite. 3048. Dark grey glassy slag, with scattered crystals of opaque yellowish-green material, apparently in rhombic prisms. (Labelled SA, but not corresponding in description to No. 8, of Dr. Percy's Eeport.) 3049. Mass of greenish grey slag, no locality. This shows a surface with the ends of light coloured tetragonal prisms imbedded in a darker substance, and with a hollow in the centre of each. On the other side the crystals interlace confusedly. 3050. Similar mass of slag, with the intervening matrix in places of a deep purple blue. 3051. Piece of tlie deep purple-blue matrix alone, showing a few of the lighter greenish crystals in the centre. 3052. Piece of blast furnace slag, showing layers of different characters, no locality. At the base it is deep blue and compact, then it changes to yellowish :green, then to brownish green, becoming more crystalline and darker in tint from the inside to the outside. The crystals show complex structure and are rhombic or tetragonal and semi-transparent. 348 3053. Blast-furnace slag, crystallised in the form of augite, locality unknown. The crystals are black and interlace, leaving interspaces. They are complex prisms, having the form of augite (Miller). Communicated by Mr. Holmes. 3054. Blast-furnace slag, showing radiating crystallisation, from Dowlais Iron Works. This is a black heavy mass, porous on one side with drusy cavities, with fibrous crystals aggregated in sheaths. It has been analysed by GL J. Snelus, and has the formula R 2 O 3 . SiO 2 + 2 (3RO, Si 2 ). 3055. Crystalline slag, showing radiating structure, locality unknown. The crystals are black, and radiate from various points, like spheroids. 3056. Group of crystalline slags from the blast-furnaces of the Aberdare Iron Works. Communicated by David Price. One of these contains drusy cavities, in which are abundant black radiating crystals, pyramidal at the end, and with aborescent side-branches at angles of about 60. Another has the crystals more compact and forming on the outside convex hexagons like those of calcite and in one place a perfect hexagonal prism. The others are intermediate and show a very grey colour on the fresh surface. 3057. Series of Gehlenite slags from iron works at Falkirk, N.B. Communicated by H. Aitken, 1885. These were produced in making some large blocks of slag, from 12 to 15 tons, and are very unusual. See No. 3044. There are five pieces from different parts of the mass. That from near the centre is greyish green, and compactly crystalline, closely resembling a sanidine trachyte. This has been examined by A. Dick. That towards the centre from the bottom has large crystals, consisting of flat tables with outgrowths. The portion near the top is a complete network of such tables, having many intervening spaces. They are of greyer tint than the central mass. The other pieces near the " scurf" are similar in character but more compact. This portion has been analysed by E. Jackson. See Bauerman, Proc. Iron and Steel Institute, 1886. 3058. Blast-furnace slag resembling Gehlenite. Part of this consists of short prismatic crystals with intervals between and part of closely set interlacing lamellae. Analysed by E. Jackson. This specimen shows the junction of the two varieties. 3059. Blast-furnace slag from the Olsberger furnaces on the Rhine. Obtained from M. Krantz. It shows some oblique prisms in the drusy cavity on one side, one of which appears twinned from having adjacent faces equal in parts, though elsewhere it is scoriaceous. It is the No. 9 of Dr. Percy's Report on Crystalline Slags to the British 349 Association in 1846, p. 362. The mean analysis there given, made by Dr. Percy, is Silica - - - - 53-37 Alumina - - 5' 12 Lime - - - - 30' 71 Magnesia - - - 9 '50 Manganous oxide - - - 1*41 Ferrous oxide - - - - - 0*95 101-06 See also Percy's Metallurgy, Iron and Steel, p. 501, where the slag is said to approximate to aluminiferous augite in composition. 3060. Blast furnace slag from : the Olsberger furnaces on the Rhine. Obtained from M. Krantz. It shows short pyramidal oblique crystals confusedly intergrown. It is No. 10 of Dr. Percy's British Association Report on Crystalline Slags, p. 363. The analysis by D. Forbes shows Silica - Alumina Lime - - - - Magnesia - Manganous oxide Ferrous oxide - - 100-60 There is a little graphite on one side. 3061. Spiegeleisen-slag showing crystals. From J. Brown & Co.'s Furnaces, Atlas Works, Sheffield. Communicated by T. Blair, 1876. The slag was made while working a siliceous ore with a deficiency of limestone in the charge. The crystals are greenish and hopper shaped, they form tetragonal prisms with their corners truncated at 45. In one specimen they are tabular and brown. They occupy drusy cavities in a compact crystalline green mass, contain- ing perforated crystals as in No. 3011. Accompanying this is a brown transparent glass with a green coating. The crystals have been partially analysed by T. Blair, and contain silica 33*45 per cent., alumina 15 "70, lime 20*97, manganese oxide 21-12, magnesia 2*67, and sulphur 2*37 per cent. 3062. Blast-furnace slag showing in the cavities small brown mica-like plates, locality unknown. 3063. Crystallised blast-furnace slag from Elswick Iron Works, 1868. This is a compact rock -like mass of greenish-grey colour, composed of closely fitting, irregularly placed tetragonal prisms with dark centres. 3064. Compact and crystalline slags from the neighbour- hood of Charleroi, Belgium. One from Marchienne is massive with glassy selvages, another is black, feebly porous, and from Cuillet, with radiating crystals in hollow 350 spp.ces within, another from the same spot is still more crystalline, approaching No. 3055, and one has a black glass selvage and an equally crystalline mass within one inch of it. 3065. A series of crystalline slags from the blast-furnaces of the South Easton Iron Works, Easton, Pennsylvania. Communicated by Edward Swift, 1853. They are produced in a large stuck 12 ft. in diain. by 35 ft. high, working with anthracite and smelting the brown hematite of the neighbourhood mixed with the magnetic ore of Morris County, New Jersey. The slag was cast into pools about 4 ft. wide and 12 to 15 in. deep. The crystals were developed in most of those masses which were allowed to cool undis- turbed. Their formation ceased when the slag was run into one or one and a half ton blocks. These sings are greenish-grey in colour, com- pact and rock-like within, and the crystals are developed on the surface of drusy cavities, some of these cavities have each more than a foot in diameter at the works. The crystalline portion is accompanied by some purple blue, semi-vitreous material, like Nos. 3049, 3050, which may very probably come from this locality. The crystals have been mostly examined by Prof. W. H. Miller. The specimen labelled A. is half brown, half blue, " it exhibits the forms 111 h h k of the rhombohedral ** system, the faces are covered with a coating that renders the measure- " ment of the angles impossible." They show truncated and also double hexagonal pyramids or scalenohedra. B. The crystals are " not " capabje of measurement, being covered with a fused coating, the " greater part consists of crystals of the prismatic system. Exhibiting *' the faces 001, 1JO. There are also a very few crystals probably of " the oblique system of lighter colour than the former. Possibly these " crystals may belong to the prismatic system." The former of these consist of parallelepipeds, actually with oblique angles, and with highly curved faces, the latter are double, actually oblique, rhomboidal pyramids. C. Shows " rhombohedral crystals, they exhibited the faces 111 ard " either Oil or 211." These are the same truncated or double hexagonal pyramids, or scalenohedra as in A. D. " Shows crystals of " the pyramidal system, exhibiting the faces of the forms 001 100, " the faces are not bright enough to afford a measurement." This is a more stony mass with no glass observable, and of a dull grey (neither the green nor blue) colour. The crystals are rectangular prisms of complex origin. Of the smaller crystals, E. " is not measurable . . . " probably pyramidal," it consists of the interlacing flat tabulre like those of No. 3057, the main mass of the stone is a greyish-blue and is all crystalline : F. consists of radiating crystals starring from, various points as in .TSo. 3055, some individuals are seen to be very flat double rectangular (?) pyramids as in B. of a light grey colour : G. of similar radiating structure, the crystals are either " prismatic or pyramidal" (Miller). They consist of the same tabulre, actually rectangular but not square, some with flat surfaces truncating the pyramids : H. another example of the same character ; Prof. Miller " thinks it is prismatic " : I. a specimen of the same kind showing more perfect crystals of the " prismatic system." Some of these are perfect rhombs, others consist of a combination of a dome and an octahedron forming hexagonal outlines, others again have the apex truncated by a basal plane, forming rather thin plates : J. the same kind of crystal radiating from the same surface to which a coating has been formed : K. small crystals of the same group as A. and C., i e. of " the rhombohedral system but the angles cannot be measured " (Miller). They are double hexagonal prisms, some of which are trim- 351 cated by basal planes, others by hexagonal prisms. These stand out on one side of a mass of which the other side is highly scoriaceous : L. black crystals, actually rectangular parallelepipeds, with curved faces, some of which look flatly pyramidal, " they may be figures of the cubic system, " of the form (h k 0) " ; these are like B. : M. grey square tabulas, which are rough, like pseudomorphs, hence they belong to the "pyramidal system " but are not measurable" (Miller). It does not appear that all these varieties came from the same mass, but there is no indication from which each came. 3066. Crystalline blast-furnace slag from Rubeland, Harz ? Bright grey-brown interlocking plates with intervals bet ween. Pieces of charcoal are imbedded on the other side. 3067. Grey crystalline slag. No locality. They are labelled A., C., D.. F v and appear to belong to the same group as No. 3065. 3068. Grey blast-furnace slag with a banded glassy border. This border surrounds a hollow cavity, and shows a blue sheen when seen in certain lights. 3069. Crystalline blast-furnace slag, locality unknown. This has a free irregular surface and has crystallised in an open space, the crystals are double pyramids of the oblique system with dull brown faces. 3070. Blast-furnace slag from Espeda,], Norway. Communicated by D. Forbes. A heavy dark mass in a sheet J-in. thick, showing on one side a number of flat metallic looking crystalline flakes. 3071. Iron-slag from the Manganja Hills, Africa. Communicated by Sir John Kirk, 1862. They are small pieces of heavy black scoriaceous slag. They are produced in the process of extracting iron directly from the ore as described in Percy's Metallurgy, Iron and Steel, p. 275. ANCIENT SLAGS. 3072. Old slag from a blast-furnace at Julsrudalen, Norway. Communicated by D. Forbes. Probably between 150 and 200 years old. It is a grey within, and of a completely crystalline character, the individuals not being separable. 3073. Slag from old Norwegian bloomeries. Communicated by D. Forbes. Probably over 200 years old. It is produced in the smelting of bog iron ore in pits by means of charcoal lor the extraction of iron by the direct method, which was formerly alone in vogue, the furnaces being called bloomeries. See Percy's Metallurgy, Iron and Steel, p. 320. This is a black compact heavy mass like a basalt, which must still contain a large per-centage of iron. 352 3074. Old Roman slag from Uckfield, Sussex. Communicated by A. Nesbit. These slags were found in great abundance in a certain spot near Uckfield where iron was formerly made. They were mostly removed for roadstone. Associated with these were found coins of Vespasian and others, pieces of Samian ware, and frag- ments of bronze fibulce. Some of the pieces contained fragments of charcoal. These are black heavy crystalline slags resembling basalt, still retaining much iron. They are made from the nodules of clay ironstone which occur abundantly in the Weald clay. 3075. Piece of ancient blast-furnace slag from Ashdown Forest, Sussex. Communicated by H. Bauerman from Mr. Larking's Collection. A green opaque glass, for the most part weathered dull. 3076. Mediaeval blast-furnace slags from near Uckfield, Sussex. These are formed on the same spot as No. 3074, and have been obtained from the same source, but they differ essentially in character, being made of dark glass, with lighter lines of flow, and indicating a much more complete abstraction of the iron. Communicated by A. Nesbit. 3077. Doubtful slags from Mount Sinai. Communicated by Francis Galton. They are derived from extremely ancient Sinaitic mines, which, if these are truly slags, were worked for iron. The small fragments are black, compact, and weathered on the surface, with earthy-looking brownish patches here and there. Dr. Percy calls them "black slag, not unlike iron slag." See his Metallurgy, Iron and Steel, p. 874. 3078. Old furnace slag, locality unknown, containing frag- ments of charcoal, with rounded pieces of unmelted micaceous iron ore, the bulk being a light scoriaceous glass. MISCELLANEOUS PRODUCTS IN THE SMELTING OF IRON ORE IN BLAST-FURNACES. 3079. Black blast-furnace cinder drawn out into threads at the Dowiais Iron Works, South Wales. The black glass is blown out by the blast, which rapidly cools it. 3080. Furnace-glass and wool produced at Cwm Cefn Blast- furnace. Communicated by J. James. 1855. The glass is in fine sheets, and the " wool " in fine hair-like threads of the same greenish colour. It is a result of the slag coming in contact with the blast of the furnace. 3081. "Furnace-wool" produced when an iron smelting furnace was working badly, no \vater being present in the twyers. Communicated by Mr, Roper. It has with it numerous round blebs of black glass. 353 3082. Hair-like slag, or " furnace- wool," produced at Dowlais Iron Works. It was blown out, through the stopping, which was defective, round the back twyer of a blast furnace. Collected by Dr. Percy, 1870. It is interspersed with round dark blebs of glass. 3083. Slag-wool from the^cupola at the London and North- western Company's Works at Crewe. Communicated by Mr. Webb, 1881. 3084. "Furnace-wool," or "silicate cotton," from a blast- . furnace at Elswick, Newcastle -on-Tyne. Produced by the regurgitation of the blast. It is of a pure white colour, and has very few light transparent blebs. 3085. Hair-like form of slag from iron furnace at Kb'nigs- hiitte, Upper Silesia. Bought of A. Krantz. 3086. Three manufactured specimens of furnace-wool, which is now put to economic uses. The most inferior is like those above, with an irregular fibre and numerous glassy blebs. The second is in asbestos-like shreds, con- sisting of bundles of fibres, and is tinned with brown. The third has the fibres long, uniform, and clear white, like the finest curled silk. 3087. Slag in small round pellets blown out of a small hole in the twyer side of one of the blast-furnaces at the Ormesby Iron Works, Middlesborough-on-Tees. Communicated by F. H. Marshall, J877- Each pellet is hollow, and the^material of which the case is made is finely porous. Some are dark, but most are nearly while. 3088. Comminuted blast furnace slag, produced artificially to serve as a manure, at the Ebbw Vale Iron Works. Communicated by Gr. Parry, 1863, who has, patented the process,.. No. 476 of 1864. In the specification he states that it is produced by applying below the gutter along which the slag runs from the furnace jets of steam, obtained from the blast engine boilers, with a pressure ot' I71bs. to the square inch. The jets are made to resemble the bat's. wing burners for gas, so as to take the form of a thin sheet^ striking on the descending stream of fluid slag; by this means it is drawn out into- coarse wool, the absence of blebs being secured by an adjustment of the jet. It is afterwards powdered for use. The powdered slag is recom- mended for use in the manufacture of bricks, artificial stone or cement, and also as a mineral manure, on account of the soluble alkaline silicates it contains. 3089. Crystalline graphite from a blast-furnace at Elswick. Communicated by A. Noble, 1868. It consists of brilliant micaceous plates of large size, which have formed on the surface of a loose mas& of sand, probably the casting sand into which the pig iron runs. IJ 61955. V />, 354 3090. Artificial graphite from iron furnaces, locality [un- known. These pieces contain fragments of slag, and are mixed with metallic iron. 3091. Graphite from the iron works of Sir William Arm- strong. A solid compact mass of irregularly arranged micaceous graphite, which surrounds numerous isolated pieces of metallic iron interspersed throughout the mass. 3092. Artificial graphite from Mr. Blackwell's Iron Works, Staffordshire. Communicated by Mr. Blackwell, 1845. The mass of this is a grey grit (perhaps the " bear"), coated with large micaceous flakes. 3093. A mass of solid porous slag, with a growth of large graphitic crystals on one side, locality unknown. 3094. Graphite from the iron furnaces of Dowlais, South Wales. Communicated by Mr. Child, 1862. 3095. Graphite from the iron furnaces of Dowlais, treated for the elimination of silicon. It has been digested in hydrochloric acid, and heated in molten potash, and treated with hydrofluoric acid. It appeared to contain silicon, because when thus heated in molten potash it gave cff an inflammable gas. See Percy's Metallurgy, Iron and Steel, p. 511. 3096. Graphite from a South Staffordshire iron furnace. Communicated by T. Dawes, Bromford. Associated with loosely aggregated sand. 3097. Largely crystallised graphite from a blast-furnace at Barrow-in-Furness. Communicated by J. T. Smith. The crystalline form may be clearly seen on these, some presenting the faces of scalenohedra, or pyramids, others show a low rhombohedron. 3098. Largely crystalline graphite from the Elswick Furnaces, Newcastle-on-Tyne. Communicated by E. S- Noble, 1867. Shows no measurable surfaces. 3099. Crystalline graphite occurring as a vein in a piece of pig iron. The large plates are transverse to the walls of the vein. From Chapell Hall's Furnace, South Staffordshire. The furnace was making No. 1, or hot iron, from blackband ironstone. The molten metal ran over the dam along with the cinder, so that it had two or three inches of 355 cinder over it and one or two inches under it, and it lay undisturbed for about five or six hours. 3100. Graphite in large soft aggregated flakes, from a fur- nace at Arnaville, Val d'Aosta. Communicated by H. Bauerman, 187 L The ore smelted was mag- netite, and the fuel was charcoal. 3101. Loose graphite flakes or " kish," from the Clarence Iron Works, near Middlesborough-on-Tees. 3102. Samples of kish in its winnowed and in its crude state. The latter contains foreign fragments which get mixed up with it, but which may be separated by winnowing. 3103. Brown material accompanying kish in the cavities of pig-iron. On running out the pigs of a Middlesborough iron furnace in Sep- tember 1863, the moulds were not filled up, but the iron formed cavities at the top and sides which were found filled with kish and this material. On analysis it yields : Carbon - - - - 23-6 Silica - - - - - 49-0 Ferrous oxide - - 16-2 Manganous oxide - - - 11-7 100-5 It is thus a mixture of graphite with a ferro-magnesian silicate. Communicated by J. Lowthiau Bell. 3104. Coating of oxide of iron from hot-blast pipes. Obtained at the Russell Hall's Furnace, Dudley, 1851. The pieces are about five-sixteenths of an inch thick, and contain several concentric layers which are grey within, but red along the surface of junction. 3105. Slag which " has spontaneously disintegrated. From the blast furnaces of Workington, Cumberland. The slag, previous to its spontaneous disintegration, was grey and cellular. The powder when breathed upon gives an odour of sulphur- etted hydrogen. It occurred in a furnace in which a mixture of " hard " and " soft " red haematite was smelted with the production of grey iron (No. 3195). It is thought to be due to an excess of lime in the flux. See Percy's Metallurgy, Iron and Steel, p. 506. Communicated by W. W. Smyth. 3106. Silicate of lime in powder, produced in a blast furnace. 3107. Fume from the Stanhope Iron Furnace. A rough brown powdet, Z 2 356 3108. Sal ammoniac obtained from the gases of a blast- furnace at Ebbw Vale. Communicated by G. Parry, 1859. The consumption of raw coal instead of coke in smelting involves the elimination of the ammoniacal fases which are produced in the heating of coal. This gas has been issolved in water and the solution evaporated. See Percy's Metallurgy^ Iron and Steel, p. 475. 3109. Specimens of old 93-806 100-000 3173. Grey pig-iron, No. 1. Produced at the 'Ystalyfera. Iron Furnaces, South Wales. Finer grained at the bottom than at the top. 3174. Grey pig-iron, No. 2. Produced at the Ystalyfera Iron Furnaces, South Wales. .The grain is coarsest inside. 3175. Grey pig-iron. No. 3. Produced at the Ystalyfera Iron Furnaces, South Wales. The grain is very like that of No. 2. The ores used at these furnaces were the argillaceous ironstones of the South Wales Coal Measures with a proportion of haematite from Ulverstone. 3176. Bright iron. Produced at the Ystalyfera Iron Fur- naces, South Wales. This is closer grained than the others. 3177. Mottled iron. Produced at the Ystalyfera Iron Furnaces, South Wales. A cross fragment of a pig finely spotted grey and white, and with a very fine grain. 3178. White iron. Produced at the Ystalyfera Iron Fur- naces, South Wales, Fine grained and compact, with crystals feebly shown, radiating from the surface to meet in the centre. 3179. Grey pig-iron. Produced at the Newland Furnaces, Ulverstone, Lancashire, 1856. Communicated by Mr. Roper. A small pig of varying grain, said to- be kishy. The slag from this- -smelting is No. 2989. 366 3180. Close grey pig-iron. Produced at the Newland Furnace, Ulverstone, 1856. Communicated by Mr. Roper. Irregular in the grain. The slag from this smelting is No. 2991. 3181. "Mottley" pig-iron. Produced at the Newland Furnace, Ulverstone. Communicated by Mr. Roper, 1856. A coarse pig, with casting material imbedded, mostly composed of white iron with a radiate crystallisation from the surface, the materials in the centre being spotted with grey iron. 3182. White iron. Produced at the Newland Furnace, "Ulverstone. Communicated by Mr. Roper, 1856. A small pig entirely crystalline, the crystals radiating inwards from the surface. 3183. White pig-iron. Produced at the Newland Furnace, Ulverstone. Communicated by Mr. Roper. This is white iron crystallising from the surface, with hollow air-blown cavities. This iron is unsaleable and is the result of a long continuance of bad working, so that the ore comes down to the twyers in a raw and unaltered state. The slag produced in this smelting is No. 2995. 3184. Grey pig-iron. Produced at the Gartsherrie Furnaces. Communicated by Mr. Davis. A very fine grained iron. 3185. " Langloan " pig-iron. Communicated by Mr. Davis. A rather coarse grained crystalline iron. 3186. Pig of cast iron, showing white iron round the edges and grey iron in the centre. Locality unknown. 3187. Grey pig-iron from Dallmillington. Communicated by Mr. Davis. It is a shallow pig, and has an ex- cessively fine grain, slightly mottled with white iron. 3188. Mottled pig-iron, almost entirely white with only a few spots of grey iron near the centra Locality unknown. 3189. White iron showing radiating structure. The surface is nearly an accurate circle whose centre is at the spot whence the crystalline fibres diverge with the greatest regularity. 3190. Vesicular pig-iron. Produced at Russell Hall's Fur- naces, Dudley. The iron is uniformly interspersed with hollow round vesicles, occupying about half the bulk of the pig. 367 3191. Pig-iron produced at the Summit Foundry, West Bromwich. Communicated by R. Farley, 1881. This class of pig is used for casting chilled rolls for rolling sheets of iron. 3192. Mixture of iron. Produced at the Summit Foundry, West Bromwich. Communicated by E. Farley. A special mixture used for rolls that are required for rolling steel plates. It is of great tensile strength, and will stand expansion and contraction. 3193. Iron called " Hange Pig." Two samples. Moderately fine grained. 3194. Mottled iron. Produced at Ystalyfera Iron Furnaces, North Wales. A shallow pig the border of which is radiately crsytallised white iron, the interior for more than half the bulk is granular grey iron. 3195. Pig-iron in two varieties. Produced in the furnaces of the West Cumberland Haematite Co. The iirst variety is of a lighter colour than the second. They are made from a mixture of the hard and soft haematite with Marlyhill coke, using the hot blast. 3196. Common white forge pig-iron. From the Dowlais Furnaces, South Wales, 1871. A broad shallow pig, of a light tint, but showing no crystallisation, and perfectly and finely granular. 3197. Small piece of white pig-iron. From the Cyfartha Iron Works, South Wales, 1859. One side shows a pitted surface, with round depressions, like the prints of rain drops, on the other are some minute conical protuberances like icicles. 3198. Ballast pig-iron from Portsmouth Dockyard. A broad mass of mottled cast iron with a coarser mottling on one side than on the other. 3199. Two samples of pig-iron made at Whitehaven Furnaces, from the Cumberland haematite, one by the aid of fluxes and the other without. Communicated by W. Randleson, 1851. Sample No. 1 has been smelted without the fluxes. It is found to be irregular in structure, very compact externally, and fibrous and loose internally with a red tinge probably due to unreduced ore. It is also found to be weaker. Sample "No. 2 is from the same ore treated with usual limestone flux and is more regular in the grain. 368 3200. Pig-iron said to be rich in silicon. Used in producing gun-steel by the open hearth process at the Arsenal, Woolwich. Procured in 1884. Exteriorly it is a white iron, within there are drusy cavities "lined with brilliant black crystals, of undetermined nature. 3201. Pig-iron from the Whitehaven Haematite Iron Com- pany, Cleator Moor. Analysed by C. Tookey, gives-- Carbon - 2-99 Silicon - 2-60 Phosphorus - 0*05 Sulphur - 0-16 Manganese , 0-56 Iron - - - US - 93-64 100-00 3202. Pig-iron, No. 1. Analysed for Messrs. Cammel, 1874. It contains 5-71 per cent of silicon, 3 '46 per cent, of carbon (com- bined or uncombined), and 0-43 per cent, of titanium. 3203. Pig-iron, No. 2. Analysed for Messrs. Caramel, 1874. It contains 5-81 per cent, of silicon, and 3-46 per cent, of carbon. 3204. Pig-iron, No. 3. Analysed for Messrs. Cammel, 1874. It contains 5 '375 per cent, of silicon, 36-44 per cent, of carbon, and 0-22 per cent, of titanium. 3205. Pig-iron, No. 4. Analysed for Messrs. Cammel, 1874. It contains 5-35 per cent, of silicon and -3-57 per cent, of carbon. All these four pigs are of grey iron with a uniform rather fine grain. 3206. Pig-iron made from hard haematite ores and containing 2'2 per cent, of silicon. From the Whitehaven Haematite Com- pany's Furnaces. 3207. Pig-iron made from soft haematite .ores, and containing 1'87 per cent, of silicon. From the Whitehaven Haematite Company's Furnaces. 3208. Pig-iron made from a mixture of hard and soft haema- tite ores and containing 2 64 per cent, of silicon. From the- Whitehaven Haematite Company's Furnaces. Of these irons all are grey, the first two are fine grained, the last is coarser. 3209. Pig-iron containing 7-5 per cent, of silicon. Front Dowlais Furnaces, South Wales. Communicated by E. Riley, 1859. It was made many years pre- viously from a very weak black band of the Coal Measures. It is very 369 white in tint and said to be very fluid when melted. The amount of silicon confirmed by W. Weston. 3210. Pig-iron rich in phosphorus. Communicated by F. Abel, 1859. The portion which remained longest melted, and consequently which was the last to solidify, contained the most phosphorus. The larger piece shows an external coating of white iron and the inner part is grey. The small piece belongs entirely to the outer coat of white iron. 3211. Filings of pig-iron. Analysed by W. Weston. Locality not stated. It contains Iron - - - Graphite Silicon - Sulphur Phosphorus - Manganese 99-86 3212. Iron said to contain 19 per cent, of silicop. It is acted on with great difficulty by hydrochloric acid. Communi- cated by W. Flight, received from Lawrence Smith, United States, 1880. 3213. Illustration of the working of ilmenite as an ore. Consisting of a mass of ilmenite, a fragment of a cast iron bar pro- duced from it, which is fine in the grain and mottled in colour, and the slag which accompanies it, which is opaque, glassy, and tinted with blue.. Communicated by E. Riley. 3214. Pig-iron remelted, said to contain phosphorus. Two samples communicated by J. P. Marrian, Birmingham. Both show a copper-coloured tarnish, one is "scoriaceous and has arborescent crystallisation, the other is still more copper-tinted. 3215. Sample of chilling iron, cast at the London Road Iron Foundry, Edinburgh. Communicated by H. Louis, 1880. It is a mixture of several different kinds of pig-iron, and shows a remarkable change from grey to white iron, passing from one side of the ingot to the other. The white fibrous crystallisation dies out amidst the dark grey particles. The white iron is more compact on the exterior surface than the grey. On analysis, before chilling the mixture yields Graphite - 3-0 Carbon combined - 0-5 Silicon - 1-0 Phosphorus - 0-3 Sulphur - - 0-1 U C1955. AA 370 Manganese Iron - 100-00 3216. " Llynvi " iron, recast from the pig. From ironworks near Bridgend, Glamorganshire. The iron is chiefly smelted from the black band ironstone of the Coal Measures. It is very red short. Communicated by Mr. Crawshay. 3217. Specimens illustrating experiments on chill-casting of iron in Portsmouth Dockyard. Communicated by W. Weston, 1868. The castings are from the mottled ballast iron, No. 3198. Two of them were cast in sand, the one from the most mottled iron still showing some mottling in the centre ; and two are cast in metal, in which the iron has a crystalline fracture radiat- ing from the surface. FOREIGN PIG-!BONS. 3218. Light fluid iron, made from bog-iron ore. It is cast in a small ingot, and is said to be very brittle and only to be used when mixed with grey iron. Obtained from A. Krantz. 3219. Crystalline white iron, smelted from Elba ore, by means of charcoal. Communicated by Messrs. Hunt of the Brades, 184ft. 3220. White rough iron. From the Grosteiner ore, smelted at Malapane, Upper Silesia. A piece of a small ingot. Obtained from A. Krantz. 3221. Iron made from chrome iron ore in Upper Silesia. A small porous fragment of a pouring. Obtained from A. Krantz. Examined by A. Dick, and found to contain no chromium. 3222. Iron from the Gleiwitz Furnace, Upper Silesia. Obtained from A. Krantz. It has been for a whole year in a fluid condition. It is now coarsely crystalline. 3223. Pig-iron from Finspong, Ostgothland, Sweden. Communicated by C. Eckman. Gothenburg, 1848. It is a turning out of a cylindrical mass, broken across to show the fracture. This is mottled white and grey ; the white iron forming a network seen on the cut surface. 3224. A second example of pig-iron from Finspong. In this there is more grey than white iron. 371 3225. A third example of mottled pig-iron from Finspong. This shows extremely well the mottled appearance produced by the white iron forming a network in which the grey iron is enclosed. This iron is only used for ordnance purposes. It contains a notable proportion of sulphur ; in fact, some ore containing pyrites is in- tentionally added to the charge in order to supply the iron with sulphur, which adds to its strength. See Percy's Metallurgy, Iron and bteel, p. 554. A similar structure has been intentionally produced by adding sulphide of iron to grey pig-iron. See Percy's loc. cit., p. 133. 3226. White iron from a Swedish furnace, showing a very coarse crystalline fracture. 3227. Swedish charcoal pig-iron from Bjorneborg. Communicated by C. Sandberg. It is made from the Persberg ore, and has been cast into a flat iron dish. The portion which has cooled in contact with the bottom and side has produced white iron, which is in large crystals, separated by a sharp line from the granular grey iron of the upper surface. 3228. Swedish pig-iron, cast in an iron mould, and showing distinct separation of the grey and white iron. Pos3ibly from the same casting as the last. 3229. Pig-iron from the Finspong Iron Works, Norkoping, Sweden. Examined by W. J. Ward, and found to contain copper, 1 365 per cent. 3230. Pig-iron cast in chill, at the Finspong Iron Works, Norkoping. Analysis by Andreas Gull. It contains Iron - Manganese Alumina Lime - - Magnesia - Silica - - .;-'. Carbon Phosphorus - Sulphur 100-83 This, therefore, notably differs from the previous on-^s in the almost total absence of sulphur. It has been re-cast ; the sides and base are white, the centre is minutely mottled ; but all is of very fine grain. 3231. Fragment of grey pig-iron brought from India, and said to be of very good quality. It is 'dark and very finely granular. A A 2 372 3232. Pig-iron from Madras, called "grey." It is part of an ingot, almost entirely composed of white iron, with a long crystalline fracture. 3233. Foundry pig-iron, No. 1. Produced at the Dunbar Iron Works, Pennsylvania. It is smelted from J Lake Superior ores, and " Native " ores, and cast in a large pig, with coarse fracture. 3234. Foundry pig-iron, No. 1. Produced at the Dunbar Iron Works, Pennsylvania. It is smelted from i Lake Superior ores, f " Native " ores, and -J mill cinder. 3235. Foundry pig-iron, No. 2. Produced at the Dunbar Iron Works, Pennsylvania. It is smelted from i Canadian ore, 4 mill cinder, and the rest of "Native "ore. 3236. Standard forge pig-iron. Produced at the Dunbar Iron Works, Pennsylvania. It is smelted from i Lake Superior ores, f Canadian .ore, and f "Native" ore. It is of finer grain than the foundry pig irons. 3237. No. 2 iron from the Iron Works of Newark, New Jersey. A very finely crystalline white iron ; the fibrous crystallisation not been visible in a fracture transverse to the length. This is originally derived from franklinite, an ore of zinc (see No. 1255), which after extraction of the zinc (see No. 2930) is treated for iron. ANCIENT PIG-!RONS. 3238. Ancient pig-iron from the Forest of Dean. This is the grey iron which was made in the Forest of Dean in the 16th century, probably very soon after the discovery of pig-iron had been made. Communicated by D. Mushet from Col. Yorke's collection. The next is the accompanying slag. 3239. Blast furnace slag from ancient iron smelting works of the 16th century in the Forest of Dean, Associated with the pig-iron above. It is partly groenish-grey> and compact, and partly a purplish glass. From Col. Yorke's collection. 3240. Chips of cast iron belonging to the 14th or 15th century. These small pieces were chipped from the interior of a bombard of the 14th or 15th century; found in the ditch of Bodiham Castle, and afterwards exhibited at Battle Abbey. Its bore was 15 inches, and it 373 was strengthened externally by wrought-iron hoops. These pieces of cast iron prove the discovery of that material as distinguished from wrought iron, prior to the date named. Communicated by J. H. Lefroy. SPIEGELEISEN. 3241. Spiegeleisen from Messrs. Bird & Co. Very white and well crystallised with a dark tarnish. Analysed by W. J. Ward. It contains : Carbon - - - - 5-0.5 Silica - - - - 0-23 Phosphorus - - 0-04 Sulphur - - 0-01 Manganese - - - 2-96 Iron by difference - 91*71 100-00 3242. Spiegeleisen from Rudolf, Wolff & Co. With a very bro\vn tarnish. It contains 7-25 per cent, of man- ganese. 3243. Spiegeleisen from Mr. Attwood. From Tow Law Works, Durham. Examined by W. J. Ward. It contains 2-16 per cent, of manganese. Compare the analysis of a similar specimen by W. J. Ward in Percy's Metallurgy, Iron and Steel, p. 534. 3244. Spiegeleisen from Dowlais Iron Works, South Wales. Analysed by W. J. Ward. 3245. Spiegeleisen, containing 12 '7 per cent, of man- ganese. Communicated by E. W. Harvey. 3246. Spiegeleisen manufactured frum the residue of Franklinite at Shirley Works, New Jersey, U.S.A. Communicated by J. Bauerman, 1866. See an analysis of a similar specimen in Percy's Metallurgy, Iron and Steel, p. 534. 3247. Spiegeleisen showing well marked crystalline forms. Communicated by John Brown & Co., Atlas Iron Works, Sheffield. Some of the forms closely approach oblique rhombs. 3248. Spiegeleisen from an unknown locality. 3249. Mass of cast iron resembling Spiegeleisen uninten- tionally produced at the Longton End Iron Works, Longton, Staffordshire. The furnace was charged with one third of Froghall Hydrate ore, about one third of " Bassy and Red " Mines, and one third the lean 374 ores of the neighbourhood, the fuel was the " ash " of the neighbour- hood, with a small proportion of Durham coal. Communicated by J. Goddard and Sons.- 3250. Another specimen of the same accidental spiegeleisen, showing flat thin crystalline plates. 3251. Spiegeleisen with a crystalline surface of thin iridescent laminae which cross each other. Communicated by the Bowling Iron Co., Bradford, Yorkshire. From a German brand of spiegeleisen " au." On analysis the bulk was found to contain 0*32 per cent, of silicon, 0-023 per cent, of sulphur* 0-096 per cent, of phosphorus, and 10-71 to 10-78 per cent, of manganese. 3252. Spiegeleisen with large surface crystals of thin tabular form, which are coated over with some crystals of graphite which have separated out on cooling. Communicated by Dr. L. Beck, Darmstadt. 3253. Spiegeleisen with very well defined cleavage surfaces. Locality unknown. 3254. Spiegeleisen made at Landore from Carthagena ores. It contains about 10 or 12 per cent, of manganese, and 3 or 4 per cent, of silicon. Communicated by H. E. Hackney. 3255. Specimens of spiegeleisen in the form of large separate plate-like crystals. 3256. Oils obtained by the action of sulphuric acid on spiegeleisen. The deep coloured oil is the crude oil, the rest have been separated by distillation, and came off respectively at the temperatures 200-210 F., 210-230, 230-250, 250-270, and above 270 F. Experiments by C. Tookey. SPECIAL CRYSTALLISATIONS OF IRON. 3257. Cast iron crystallised as an octahedron. Communicated by G-. Matthey, 1871. It has a rough surface, and is of complex origin. 3258. Cast iron artificially crystallised in octahedra. From the DemidofF Iron Works, Siberia, 1880. The octahedra occur in a drusy cavity, and are mostly striped parallel to the sides by a succession of growths. 3259. Section of coke-pig, produced by hot blast at the Londonderry Furnaces, Nova Scotia, showing here and there, some octahedral crystals. Communicated by H. Louis. 375 3260. Crystallised pig-iron, produced at the Russell Hall's Furnaces, Dudley. Communicated by S. H. Blackwell before 1851. It is a surface formation of rectangular crystals occasionally arranged in an arborescent form. 3261. Arborescent crystals of cast iron, from the centre of a block cast for the fortifications of Todleben, 1880. 3262. Arborescent crystals of cast iron, from Staffordshire. 3263. Arborescent crystallisation in cast iron from the Clyde Iron Works. Communicated by D. Mushet from Col. Yorke's collection, 1875. These crystals are so arranged as to form in many cases skeleton octahedra. 3264. Crystallised pig-iron, locality unknown. This is not arborescent, but consists of numerous skeleton octahedra placed one on top of the other so as to form a tetragonal pyramid, which is terminated by the final octahedron. 3265. " Kishy " pig-iron with large crystals. From the Newland Iron Furnaces, Ulverstone, Lancashire. Com- municated by E. Roper. This is obviously not from a regular pig, but a portion of the iron which did not go into the moulds ; it contains a piece of imbedded stone. 3266. Very largely crystalline cast iron. From the Elswick Works, 1868 ? The surfaces are brilliant ; they meet at acute angles, and have their faces obliquely striated, and there is nothing to show them to be isometric. The fragment is not from a pig, but from a flat cake, and it contains several pieces of imbedded stone. 3267. Very largely crystalline cast iron. From the Elswick Works, Newcastle -on-Tyne, 1867. Communicated by E. S. Noble. This is also from a flat mass, the crystals on one side are immense. Their faces are striated by two sets of lines, making angles of 60 as though the system was hexagonal. The other side has the ordinary fine crystals of grey iron. 3268. Kishy iron produced at the Blaina Iron Works, Newport, Monmouthshire. Communicated by J. F. Davis. The metal shows coarsely crystalline plates, or a graphitic appearance, and crossed by lines making angles of 60 with each other. It occurred when the burden was very light ; and composed of Redmine calcined ironstone, a small portion of burnt cinders and very strong coal and coke, the furnace working with hot blast. The iron adheres firmly to a coating of slag. 3269. Pig of cast iron, showing a layer of larger crystals at some depth from the surface. Locality unknown. 376 3270. Crystalline iron from No. 1 Furnace, Chapel Hall, Staffordshire. PIG-IRON PRODUCED UNDER SPECIAL CIRCUMSTANCES. 3271. Columnar iron forming part of the " bear " or " horse " of a blast furnace at Ebbw Vale. Communicated by G . Parry, Junr. The iron is crystalline, as seen at the ends of the long narrow columns, which are 5 or 6 sided. 3272. Iron accumulating on the bottom of a blast furnace and forming the " bear " or " horse." It shows a well-marked columnar structure. From the Ebbw Vale Iron Works. 3273. Iron from the furnace bottom at one of the furnaces at Els wick, Newcastle-on-Tyne. Communicated by E. S. Noble, 1873. It has very large cleavage surfaces, which are cracked rectangularly and parallel to, or making equal angles with rectangular strise. There are some large toles which have a golden tinge. Compare No. 3122. 3274. Iron from furnace bottom at one of the furnaces at Elswick, Newcastle-on-Tyne. Communicated by E. S. Noble, 1873. This, though from the same works, is not brilliant like the last, but has a kishy appearance. The cleavage planes meet obliquely and the striae make angles of 60 with each other. The under surface is covered with graphite. Com- pare Nos. 3266, 3267. 3275. Crystallised iron from the " bear " of a blast furnace. It is very white, and shows columns ranged parallel to the top and bottom surfaces. 3276. Very columnar iron from the " bear" of a blast furnace. The long narrow columns are parallel to the upper and lower surfaces. The iron is very white in colour. Some wrought iron made from this accompanies it. 3277. Piece of the old "horse" from Gwyther Forge, Abercarn. It is a finely granular white iron. Produced by charcoal. 3278. Piece of an old "bear" from Bilston Furnaces, Staffordshire. It shows a curved columnar structure, more or less perpendicular to the surface of the bear. It is produced by long continued heat. Communicated by S. H. Blackwell, 1856. 377 3279. Portion of a remelted "horse" from the bottom of a blast furnace at Wolsingham, near Darlington, containing an extraordinary proportion of silicon. Communicated by Chas. Atwood, 1867. It has a peculiar grey lustre, aud is frothy and porous. It has been described by Dr. Percy in the* Transactions of the Iron and Steel Institute. The furnace had been long in blast, and this was the last portion that melted on increasing the blast and adding coke and lime in order to clear out the bottom of the furnace. There was about 1 ton of this material. Sandstone, with iron diffused occurs in the furnace which might be reduced to silicon, It has been analysed by W. J. Ward and contains; Silicon - - - 15-378 Carbon - 0'787 Phosphorus - O'lia Sulphur - 0-088 Manganese - - 3 '425 Copper - 0-083 Nickel and cobalt - traces Lime- - - 0-424 Magnesia, alumina, &c. - traces Iron (by difference) - - 79 '702 100-000 3280. Portion of a bear 1 in a furnace of the Wigan Coal and Iron Co., Lancashire. It consists of numerous small round blebs of metal, now coloured bro'j n, imbedded in a matrix of blue earthy looking material, and is certainly not pure iron. On analysis it yielded Silica (including Silicon) Total carbon - Manganous oxide Lime - Magnesia Phosphorus - Sulphur Iron 100-81 It has been re-fused under plate glass and the metallic portion has sunk to the bottom, and a brown glassy slag has formed at the top. The metal is of mottled iron, and consists of nodular fibrous crystals intercrossing at right angles. SLAGS PRODUCED IN THE FINING OP PIG-IRON TO OBTAIN WROUGHT IRON. 3281. Slag from the fineries at the Bloomfield Iron Works, Dudley. This is composed of a number of interlocking large flat plates, whose surfaces are covered with numerous dull coloured rectangular pyramids which grow one over the other. 378 3282. Slag or tap cinder. From the finery at Bloomfield Works, Dudley. This is covered with strong crests, composed of the angles of a number of overlapping pyramids, whose other edges stand out from the side. 3283. Large mass of slag or tap cinder from an iron finery. Locality unknown. The surface of this slag is covered by numerous crests in the form of oblique rhombs, which are made up of a number of pyramids ranged in lines and overlapping, which gives them a grooved appearance, and each of these minor crests is itself made up of smaller pyramids. The body of the slag is compact, but crystalline in parts. It is divided into several partial layers by bands of gas holes, which are lined with a silvery coat, which also covers the crystals here formed. The under side, is covered with excessively low oblong pyramids, the remoter parts of which are covered with the ,ame silvery covering. 3284. Iron finery slag from an unknown locality. The surface consists of large narrow crests, which are built up of similar plate-like crystals lying close together, the centre one extending furthest, Each plate is also complex and has the form of a very low pyramid. A section of the under side of this specimen has been taken for microscopical examination. 3285. Another specimen from the same mass. This shows the same crest-covered surface, but the crests are com- posed of numerous pyramids, whose solid angles jag their edges as in No. 3282. 3286. Another specimen from the same furnaces. The surface is not here in crests, but in peaks, by the superposition of the pyramids round a vertical line. 3287. Another specimen from the same furnaces. The broad surface of the thin plates or low pyramids seen in No. 3284 is here along the top of the slag, which is covered with these scale-like crystals. 3288. Another specimen from the same furnaces. In this, which is a thinner mass, the low plate-like pyramids are arranged nearly parallel to the surface, which they merely ridge in different directions. 3289. Another specimen from the same furnaces, The surface is covered by very narrow brilliant crests, standing vertically. They are the separate low pyramids, not combined into large ones as in No. 3284. 3290. Finery slag from another furnace. Locality unknown. It has several spiny outgrowths consisting of superimposed octrahedra. 379 3291. Finery slag. Locality unknown. Its surface is covered with medium sized crests, which stand vertically. They are each composed of a complexity of linear crystals arranged obliquely. 3292. Calcined cinder from the mill. Locality unknown. These are covered with numerous perfect pyramids belonging to the oblique system. They are coated with a brown deposit which renders the faces dull. 3293. Scoriaceous cinder. Locality unknown. This is full of holes on the under side, but on the surface are numerous dull crystals of forms belonging to the rhombic system, mostly rectangular pyramids, but sometimes a combination of several forms. 3294. Calcined tap cinder. A scoriaceous mass of inferior quality, containing 77-81 per cent, of ferric oxide and no ferrous oxide. 3295. Calcined tap cinder. A scoriaceous mass of superior quality. It contains 86 48 per cent, of ferric oxide and a scarcely appreciable quantity of ferrous oxide. These two have been determined by R. Smith. 3296. Tap cinder. Communicated by Mr. Kitson. Semi-scoriaceous-below, but in the open cavities covered with brilliant black orthorhombic pyramids of small size. 3297. Tap cinder calcined. From the Brader Works, Old- bury, 1861. A scoriaceous mass, all the cavities are lined with minute, but brilliant black crystals, in the form of orthorhombic pyramids. These are said to be of " iron olivine." 3298. Iridescent tap cinder from the Blaina Iron Works. This appears to be partly composed of the sand of the hearth, on which was condensed here and there some blue material (salt of copper ?) passing at its edges to purple. 3299. Calcined tap cinder called " bull dog " when used for the bottom of a puddling furnace. Burnt in a kiln at Ebbw Vale, 1865, according to Barrows and Halls patent. A scoriaceous mass with blue coated cavities. 3300. Calcined tap cinder or bull dog, broken up by crush- ing between rolls. It is used in this state for fettling the puddling furnace. 3301. Crystallised slag in layers. Locality unknown. In the centre the layers separate and crystals are formed, they appear to be octahedral, but are too ill-formed for determination, the whole has a bluish tinge. 380 3302. Mill furnace slag showing iron olivine crystals. From the Warrington Wire Company's Iron Works, 1871. Contains minute iridescent crystals apparently of the rhombic system coating a shallow depression. 3303. Crystallised tap cinder. Showing coarse vertical crests, each of which is serrated by the parallel edges of a number of overlapping skeleton pyramids (labelled 12a, stated to have been analysed by Dr. Percy, but it does not corre- spond to the No. 12 of his Report on Crystalline Slags). 3304. Crystalline tap cinder. Locality unknown. The surface is composed of dark dull oblique pyramids like those of No. 3292. 3305. Crystals on the surface of a tap cinder. The bulk is slightly scoriaceous, on the surface are some isolated dull crystals showing very perfectly the double-ended oblique pyramids. 3306. Crystalline tap cinder. Apparently calcined, being very scoriaceous, the small crystals coating the upper parts and the cavities. They consist for the most part of orthorhombic pyramids, truncated by basal planes. The figure is given in Dr. Percy's Report on Crystalline Slags (Brit. Assoc. Rep., 1846, p. 366), and is best seen in this specimen. 3307. Crystals of silicate of iron of the formula 2 FeO, SiO 2 , on the surface of a finery slag. From the collection of Col. Yorke. The slag is very thin and the surface is coated with projecting black crystals of the form of thin rhomboid plates. 3308. Crystalline tap cinder. Showing tabular crystals of t( iron olivine " bevelled by the faces of a pyramid. 3309. Magnetite crystals on the surface of a calcined heap of refinery forge and mill cinder from Blaina Iron Works, South Wales. Communicated by Mr. Hoffman, 1858. They are in the form of rhombic dodecahedra, with brilliant faces. 3310. Stony mass in the form of a finery slag from Blaina Iron Works. Communicated by C. Hoffman. It is dark and cavernous, the surface is covered with brown pseudomorphous oblique pyramids, many of which are skeletons, but they are not at all metallic when broken. With this is a large crystal, equally pseudomorphous, consisting of a double pyramid on an oblong base with an oblique axis. 3311. Spherical hollow globules of magnetic oxide of iron. These are produced in large quantities in the fining of iron when jets of atmospheric air are made to impinge at a steep angle upon 381 molten cast iron. They are strongly attracted by the magnet. Analysed by R. Smith. Ferrous oxide - 28-91 Ferric oxide - 37*44 Silica - 24-10 Alumina, with smajl quantities of lime and magnesia, &c. - 9-55 100-00 From the Blaiua Iron Works, Cyfartha, South Wales. See Percy's Metallurgy, Iron and Steel, pp. 21 and 624. 3312. Shot-like slag projected from the finery furnace at the Bowling Iron Works, Yorkshire. Communicated by Mr. Gilchrist, 1871. They are all of them. hollow and black. 3313. Compact finery-slag, with a surface of small rhombic crystals referred to " iron olivine." Very brilliant and iridescent ; either plate-like or domed. 3314. Minutely crystalline piece of finery-slag. Examined by Professor Miller, who reports the crystals to consist of octahedra of magnetite, with small needles, which are an aggregation of transparent crystals of the form of olivine, but they attract the magnet. Some of the magnetite crystals are a combination of the octahedron and rhombic dodecahedron. 3315. Group of crystals from a finery-slag. These are the transparent plates of a brown colour, which cross each other. Examined by Professor Miller, who reports that they have the form of olivine, with a very distinct cleavage parallel to one face, but the angles differ slightly from those of ordinary olivine. 3316. Crystalline slag from the Urals. A scoriaceous mass, with a few dark crystals like those of olivine. 3317. Crystalline slag from the Urals. A very open mass of loosely aggregated crystals. They are black and brilliant, with the form of an oblique pyramid. 3318. Crystallised tap cinder from the iron works of the Steel Company of Canada, Londonderry, Nova Scotia. Communicated by H. Louis. It is formed in the interior of some containing case, from which the compact portion crystallises radiately ; the surface has numerous ill-defined brilliant crystals in a combination of the pyramid and basal plane, like those of oliviue. 3319. Another example from the same sxmrce, more per- fectly crystallised. 382 3320. Another example from the same source. Some of the pyramids are truncated, some are modified into domes. The crystals are produced by allowing the tap cinder to cool slowly. They have been analysed by H. Louis, and are found to contain 54-34 per cent, of metallic iron and to consist of Silica Alumina Ferric oxide - Ferrous oxide Manganous oxide Lime- Magnesia Phosphoric acid Sulphur 100-30 3321. Iron finery slag from Cujo, showing a crystalline surface. Communicated by D. Forbes. This appears to be the mass whence No. 3314 was taken. It is compact below, and has a crystalline surface of minute aggregated octahedra of magnetite. 3322. Another specimen from the same source. This consists of a compact mass below, with about 1 inch loosely crystalline, in serial portions of narrow plates and octahedra which cling to them, the plates crossing irregularly. 3323. Another specimen from the same source. This is from the end of a flow. The plate or needle-like crystals are confined to the under surface and the compact portion, and the octa hedra alone cover the upper surface, where they are very minute. The olivine seems to form where there is least access of oxygen, the magne- tite where there is most. 3324. Finery slag from Blaina Iron Works, Newport, Mon- mouthshire. Communicated by C. Hoffman. It consists of brilliant black crystals of orthorhombic pyramids, which are in some cases slightly oblique. 3325. Another example from the same source. This is the mass from which the portion examined by Professor Miller was taken, No. 3315. It consists of intercrossing plates. 3326. Crystalline finery slag ? Locality unknown. Consists of fibrous radiating crystals of a brilliant black colour, with a very irregular surface. 3327. Finery slag showing crystals of magnetite from a foreign locality. In well developed, dull octahedra. 383 SLAGS PRODUCED IN THE PUDDLING FURNACE. 3328. Refinery cinder produced in puddling cast iron to form steel at the Ebbw Yale Iron Works, 1865. The slag is thm, and has an upper surface composed of very thin vertical plates, scarcely crystalline in shape; imbedded amongst them are some several spherical shots of iron. 3329. Bottom of a puddling furnace, at the Low Moor Iron Works, Yorkshire, 1868. This shows the total thickness of the bottom. It is porous in the interior. 3330. Refinery slag from the Bromford Iron Works, near Oldbury, 1845. One piece is a solid mass with a crystalline coating in one place ; the crystals not very brilliant combinations of rhombic dodeeahedra with the octahedron, or of the cubic system, with possibly some rhombic crystals. The other pieces are covered with very minute brilliant crystals, some being prisms, others octahedra. 3331. Refinery slag from an unknown locality. These show very large crystals more than half an inch in length, consisting of a rectangular pyramid, modified by a basal plane, as in the crystals of iron olivine, seen in No. 3320. 3332. Slag from an unknown locality. A thin compact mass, with crystals standing vertically to its surface, which are flat rectangular plates, with the edges bevelled by the sides of a pyramid. 3333. Refinery cinder from the Bromford Iron Works, near Birmingham. Communicated by J. Dawes, 1845. This appears to be No. 13 of Dr. Percy's Report on crystalline slags to the British Association, 1846. It is there stated to be from the flue of a puddling furnace, where it had been exposed to a high temperature for a considerable time. The surface is covered with brilliant iridescent black crystals, having the form of thick plates, with the edges bevelled by the sides of a pyramid, or ocasionally of a prism. They belong to the rhombic system. An analysis of this slag by Dr. Percy gave Silica - 29-60 Ferrous oxide - 48-43 Ferric oxide - 17-11 Mauganous oxide - 1-13 Alumina - > - 1-28 Lime- ^ mri '-- '47 Magnesia - - 0-35 Phosphoric acid - 1-34 Sulphide of iron 1-61 101-32 See also Percy's Metallurgy, Iron and Steel, p. 668. 384 3334. Refinery slag from the Bromford Iron Works, Old- bury, 1845. Communicated by J. Dawes. An outgrowth of brilliant iridescent black crystals, each having the form of a skeleton rectangular pyramid, and so overlapping and combined as to form other complex pyramids. The crystals are essentially of the same character as in the last. 3335. Refinery slag from the Bromford Iron Works, Old- bury, Birmingham, 1845. Communicated by ,T. Dawes. This is a very thin cake, with bits of stone and sand imbedded on one side ; on the other it is clothed with brilliant black ( crystals in the form of more or less skeleton octahedra, i^e., belonging to the cubic system. 3336. Refinery cinder from the puddling furnaces of the Ebbw Vale Iron Company. A scoriaceous piece of the bed, with the bubbles on one side pulled out into long tubes perpendicular to the smooth surface. 3337. Crystallised cinder from the Bottom of the puddling furnaces at Dowlais, South Wales. Communicated by E. Riley, 1856. It consists of a number of thin mica-like brown plates standing vertically to the surface. The faces are striated with lines which form a hexagonal ; apparently belonging to the rhombic system. 3338. Miscellaneous refinery slags from the Bromford Iron Works, Oldbury. Communicated by J. Dawes. Several show very well the dull double rectangular pyramids which are here isolated. The more transparent ones'" show a deep brown colour. 3339. Refinery slag from Messrs. Solly's Works, Tividale. Obtained at the Dudley Museum. Communicated by Mr. Twamley. Of the four pieces, three have a number of crystalline outgrowths produced by the overlapping of skeleton octahedra. The fourth, which has a thicker and more irregular basis is composed of the rectangular pyramids. The two systems of crystallisation are both represented here. A specimen is referred to by Dr. Per'cy in his report on Crystalline Slags, 1846, and in his Metallurgy, Iron and Steel, p. 669, as communicated by Mr. Twamley, for the Bloomfield Iron Works, Tipton. The fourth of these specimens may be the one there referred to. 3340. Crystalline slag from a puddling furnace at New Bradford, Massachussets. Communicated by Josiah Cooke. This has large crystalline plates standing vertically from the surface. They are composed of very thin plates, aggregated into groups or formed to build up a very low rec- tangular pyramid. They are also dotted all over with little hexagonal plates of equal hardness with the rest. 385 3341. Another specimen from the same locality. This shows the plates aggregated in parallel lines which combine to form larger plates with the edges truncated by rectangular pyramids of a higher angle. The little scales are arranged in the intervals. The lower pyramids are seen on the other side. 3342. Refinery slag from the Bromford Iron Works, Old- bury. Communicated by J. Dawes. A very compact slag with an even surface sparkling with small crystals which have the octahedral form of magnetite. 3343. Slag from a Siemens' steel-melting furnace. From the Dowlais Furnace, 1871. This furna.ce was allowed to cool down with the charge in it. Com- municated by D. Watson. These are nearly transparent thin mica-like plates of a siliceous slag, obtained in smelting the steel direct from the ore. 3344. Refinery slag from an unknown locality. This has an arborescent growth composed of innumerable small well developed octahedra. Associated with these are some long prismatic crystals of small size. 3345. Slag from the melting pots of steel when manganese was used. Communicated by E. F. Sanderson, Sheffield, 1857. It is a semi- translucent green glass with cavities. 3346. Crystalline slag from a steel furnace from Cheddle. Communicated by W. W. Smyth. The crystals are large and have the form of a rather low rectangular pyramid, but they have their edges rounded and possess a peculiar silky lustre, owing to the striation of their surfaces, though they are brilliant within. Another specimen shows thin and brilliant plates. On analysis they have yielded Silica - Alumina - Ferrous oxide - - - - Manganous oxide - Lime ----- 102-76 3347. A crystallised mass of iron silicate produced from the smelting of forge cinder and coal to make " bull dog." A very large heap of forge and other cinder was mixed in alternate layers with pieces of coal, and the whole was ignited. It failed to pro- duce a suitable " bull dog," and the heap became an agglomerated and worthless mass, which could only be broken up by blasting. At the Blaina Iron Works, 1859. The drusy cavities of the mass are covered with brilliant black crystals having the form of oblique pyramids on a rectangular base. U 61955. B B 386 3348. Iron slag from an unknown locality. From some refining process. It is u black heavy mass with one side coated with dull crystals having the form of a rectangular pyramid of the rhombic system. 3349. Iron slag, locality and process unknown. It is a dark compact mass, with innumerable crystal needles crossing- in every direction. Its surface shows similarly intercrossing crystalline- plates with no well-defined outline. ' 3350. Fused oxide of iron taken from the regenerator of one of the furnaces at the Landore Siemens' Steel Company's Works, near Swansea. Communicated by A. Willis, 1872. A thin mass of slag-like material with an irregular surface coated with a bloom of excessively minute crystals. 3351. Mass of iron slag melted and poured into a cardboard box. It shows a crystalline surface in the centre, composed of very finely arborescent minute octahedra. Locality unknown. SLAGS FROM THE REHEATING FUENACE. 3352. Flue cinder from the Low Moor Iron Works, 1876. A moderately thin mass, quite compact, with crystallisation crossing- in lines from top to bottom. It has a bluish tinge of colour. The flue cinder is the material that flows out from the reheating furnace into the flue from whence it escapes. 3353. Flue cinder from the Low Moor Iron Works, York- shire, 1868. This has a narrow band of scoriaceous matter on cne side ; the rest ia- composed of radiating crystals, which aggregate on the drusy surface in sheaves of the form of bevelled plates, leaving each with a skeleton structure. 3354. Slag from the reheating or so-called balling furnace at the Melton Iron Works, near Wentworth, Yorkshire. Communicated by W. W. Smyth. It contains small rhombic crystals in the cavities. 3355. Flue cinder from Mr. Beasley's Furnaces, Smethwick, near Birmingham, 1851. A metallic-looking mass with large cavities, the interior of which is lined with crystals. These are the plate-like rhombic crystals with the edges bevelled by a rectangular pyramid, as in No. 3340. 3356. Iridescent flue cinder from Barrows and Hall's Fur- naces, Tipton, Staffordshire, 1846. A compact mass, with the under side containing numerous imbedded stones and rubbish, the upper side smooth and shining from the surfaces 387 of numerous small crystals, when seen by reflected light at a certain angle. The larger of these crystals have the form of an excessively low rectangular prism, whose vertical height, in fact, is approximately zero, and only marked out by its division into four triangles, the alternate pairs of which have a distinct colour, either blue or pink ; the smaller crystals are hexagonal on the outside, flat, and of a golden iridescence. 3357. Another piece of flue cinder similar to the last. Probably from the same source. The crystals on the surface are larger and less iridescent. They are all striated parallel to the base of the pyramid. 3358. Iridescent flue cinder. Locality unknown. The iridescence in this case is from bluish to yellowish -green. It is confined to crystals showing the ' pyramidal faces. Those which show the edges are greyish-brown. 3359. Piece of flue cinder from an unknown locality. Like the next, but smaller. The angles of the smaller piece have been measured by Mr. Brooke. The angle between the faces which are parallel to the longer diameter (i.e., that have an obtuse angle at their apex), is 168 ; that between the other faces is 173 72'. 3360. Piece of flue cinder showing a crystalline surface. Locality unknown. This has a single large crystal for a surface of more than a square inch. It is the exceedingly low rectangular pyramid seen in No. 3356. Each face is built up with partial lines running parallel to the slanting sides. 3361. Flue cinder from the reheating furnaces of Messrs. Bramah, Barrows, and Hall, 1846. A thin rather brassy looking compact mass, lined transversely, but showing no obvious crystals. One side is puckered like the surface of a flow, the other has a carpet as of very minute interwoven needles, whiclr are in reality the cross section of their micaceous plates, standing verti- cally to the surface and producing the transverse lines on the sides. 3362. Masses of scrap iron found on the floor of the rever- beratory reheating furnace at the Highfield Works, Bilston. 1881. These pieces were all found imbedded in the cinder of the charging health at about its centre, and immediately opposite the charging door. The bright parts of the iron were under the blow holes or craters in trie- cinder, but on the uppermost sides of the specimens, as found in the hearth. Communicated by J. R. Wheeldon. No. 1 was the first speci- men found on 20th of June 1881. It has been lacquered io prevent its being tarnished. The white spaces show no crystalline surface, and two or three of them are divided into parts, as a soap bubble is divided by liquid partitions, so that they appear like flattened gas cavities in a liquid. The scrap is perforated at two points, and on the back is black and nodular. No. 2 has one very large patch which is very flat. It is 6overed by the finest arborescent crystallisation. On the other side the 388 surface is covered with little pustule-like elevations, with slag in the depressions. No. 3, found four days later, shows the same arborescent crystallisations, both in the bright and dull parts, of wTiich the former have tarnished pink. It is still adhering to the cinder which is scarcely melted at an inch distant, then it becomes greenish and compact, but spongy, only at one place changing to a glass, where it passes to the other side on which lies a mass of glass occupying the dull areas, the bright ones being the continuation of the walls of gas cavities in the glass. No. 4 has in like manner some black glass fitting to the dull portions, while the bright ones correspond to its cavities. The other side has only pustules and slag. No. 5 closely resembles No. 2. It would thus appear that the heat had melted the slag above the piece of scrap into glass and produced large bubbles of gas, which being pre* vented from escaping have had an effect upon the iron. Compare No. 3283. SPECIAL PROCESSES IN THE PRODUCTION OF IRON. 3363. Specimens illustrative of Blair's process for refining pig-iron by aeration, by causing it to drop down a series of inclined steps as it flows from the blast furnace. Communicated by S. Blair, 1866. No. 1 is a sample of the pig-iron used. It is smelted with coke from Lake Superior specular ore, and fluxed with a limestone not previously used for blast furnaces. It is so strong in body and so difficult to puddle that only two heats could be made without stopping work to restore the fixing and bottom. It is ex- cessively fine in the grain. No. 2 is the same pig-iron as No. 1, but after it has been remelted in a cupola and poured down the inclined steps. This is found to work freely and more easily than ordinary coke pig-iron. It has a coarser structure. No. 3 are small tears of pig-iron poured gently into water. This was the ordinary metal used at the foundry. It requires, of course, remelting. No. 4 has also been poured into water, but has been dropped from a distance of 18 feet through the air before reaching it. The metal is all torn into agglutinated shreds. 3364. Specimens illustrating Taylor's process of stamping and assorting puddled balls. This process was patented in 1859, and carried out by Mr. Davis at the Low Furness Iron and Steel Works, Ulverstone, but has since been abandoned. No. 1 are two large lumps of puddled ball of a very open character. In this method these balls, instead of being shingled and rolled at once, are allowed to cool, then broken up under steam stamps, and then passed under rollers over a riddle, to separate the larger pieces from the smaller. These larger pieces, No. 2, are those which have been imperfectly puddled, and are called unwrought pig. They are returned to the puddling furnace, and are metallic in appear- ance, and of the size of marbles. The smaller pieces, No. 3, which pass the riddles, are more cinder-like in appearance. They are balled up and hammered, as with ordinary iron. See Percy's Metallurgy, Iron and Steel, p. 688. 3365. Illustrations of the process of smelting iron in the north of Spain. The ore used is the Camponel ore, a red haematite (1). This is mixed with a grey compact limestone found in the neighbourhood, (2), 389 and some black refining cinder (3) and Durham Coke. This compound is smelted in a hot blast furnace, the hot blast having a temperature of 350 C. only. From this is produced the piece of pig-iron (4), with a coarsely crystalline fracture, and the pieces of greenish-grey compact slag (5). This pig is afterwards refined into bars (6), about 1J in. square, which, on bending and cutting, shows a fine fibrous fracture. Manufactured at Messrs. Ebarrows Iron Works, at S. Nicholas on the River Mervion, near Bilbao. Communicated by W. E. Bell, 1872. 3366. Illustrations of Chenot's process, for the direct extraction of iron from its ores. From Ebarrows Works, S. Nicholas, near Bilbao. Communicated by W. E. Bell. The ore used is a brown oxide from Somerostro, near Bilbao, known as Galeria ore, from its being Avorked underground, in galleries (1). This is mixed in the process with charcoal dust in excess, and the whole heated to a comparatively mode- rate temperature, so as to reduce the iron oxide. It is then extracted from the base of the furnace in lumps (2), which are of a spongy character. This is used for the purpose of making steel, for which it has to be carbonised and compressed ; a resulting bar is seen in (3). For an analysis of the ore used, and a description of the processes cf reduction and carburisation, see Percy's Metallurgy, Iron and Steel, pp. 335 and 776. 3367. Iron ore reduced by Chenot's process, by Chenot himself. Procured at the Paris Exhibition in 1855 by W. W. Smyth, who was on the jury of the Metallurgical Department. It has been hammered out on one side into a projecting nail to show that it is malleable metal. SAMPLES OF WROUGHT IRON. 3368. Partially puddled ball of iron from the Bromford Iron Works. A scoriaceous looking mass. 3369. Specimen of an d contain *13 per cent, of carbon. Their composite nature is not seen on the surface. 3537. Two burglar-proof safe plates of Corngreaves' patent compo. One labelled -^ is in its soft condition, and is easily drillable. It is not composed of square bars as the other specimens, but consists of an alternation of numerous plates of iron and steel, visible on the sides. Q*7K The other, labelled Q, is the same after hardening, in which con- oo dition it is undrillable. Seven plates are seen in this on the sides, which are seen also to be laminated on the fractured end. 3538. A burglar-proof rivet, of Corngreaves' patent compo. It is bent and broken to show its structure, which consists of five square bars of steel, welded together in a matrix of iron. All these 410 specimens were communicated by Gr. Allen, of the New British Iron Company, Corngreaves' Iron Works, near Birmingham. 3539. Bars of iron and steel, piled and dra\vn out by rolling. The end has been otched with acid, so as to show the steel by the blackness thereby induced. Communicated by K. Blackwell many years previous to 1880. The different rods are arranged in section like the squares on a chess board. IRREGULARITIES IN STEEL. 3540. Piece of steel plate on which a large blister rose after it came through the rolls, at the Locomotive Works, Crewe. Communicated by F. W. Webb. The cavity has not been opened, and whatever gas may cause it may still be enclosed within the steel. 3541. Piece of blister-steel with two large hollow blisters. Produced in the ordinary process of the conversion of bar iron into steel. The fracture is coarsely crystalline, and shows a certain amount of lamination. See Percy's Metallurgy, Iron and Steel, p. 772. 3542. Piece of blister-steel with one large hollow blister extending on both sides. From Messrs. Hunt's Works, the Brades, Birmingham, 1846. The bar has a coarse crystalline fracture, and is markedly laminated at the end. The blister rises over a surface of about 2 inches by 1 inch. See Percy Journal of the Iron and Steel Institute, 1877, No. 2. 3543. The interior of a blister broken open. Communicated by Mr. Ibbetson, Sheffield, 1878. The fracture is very white, but the inside of the blister, which is thrown into folds, is lined with a blue-black coating resembling iron sulphide. 3544. Blister-steel which has been over-fired in the con- verting furnace. Portions of the bars of blister-steel are converted into grey cast iron, and these melt out from the under side and drop down on to the bars below. The amount of carbon in the melted and unmelted portions respectively have been ascertained lo be 2 '263 and 1'318 per cent. The specimens are eroded into hollows from this cause. Communicated by W. Baker, Sheffield, 1 872. 3545. Steel showing irregularities in its hardness. The specimens are cut out of discs turned off the end of a block about 13 inches diameter and 10 feet long, made of steel cast out of small pots into an iron mould and drawn out under the steam hammer. The hard spots have turned the tool in the slotting, but they are aggre- gated small spots, seen by filing. Communicated by G. W. KendeJ, Elswick Works, Newcastle-on-Tyne, 1872. 411 3546. Experimental piece of steel, treated for the purpose of testing the cause of blisters. The theory of Dr. Percy is that they are caused by the accidental, though unavoidable, presence of portions of slag in the mass which has been puddled but never thoroughly melted (see Metallurgy, Iron and Steel, p. 772). If this were sOj then a thoroughly melted bar of malleable iron which was converted by the process of cementation should show no blisters. Swedish bar iron has been melted by Mr. Frith, of Norfolk Works, Sheffield, and cast into a flat ingot. This has been converted, and the fracture of the specimen (about 6 inches long by 3 inches broad and T 7 ^ inches thick) is quite characteristic of steel, but there is no sign of a blister. See Percy, *' On the causes of Blisters in Blister- steel " in the Journal of the Iron and Steel Institute, 1877, No. 2. 3547. Piece of highly carburised steel. From Messrs* Frith's Iron Works, Sheffield, 1876. It is very coarsely crystalline in fracture, yellowish in tint, and show- numerous small blister cavities within nnd without. IRON AND STEEL SPECIALLY TREATED. 3548. Specimen of steel which has been bent and shows lamination. Obtained at the works of Messrs. Cammell & Co., Sheffield, 1882. It is part of an ingot which has been hammered and rolled cold, such as are used for making ship plates. This has been bent completely double, and then separated again. Its fracture and one side show well- marked lamination. 3549. Series of specimens of steel melted with and without manganese in order to ascertain the result of the addition, 1864. There are first two fragments of the original bar steel, labelled B. and E. V., with blisters, which have been used in the melting, a fragment of a square ingot, with bevelled edges, which has been melted without manganese, and a fragment of a similar ingot of the same size melted with manganese as usually at that time practised in Sheffield. Two larger sized tilted bars, broken to show the fracture, one from the ingot with manganese and the other from the ingot without. Two smaller bars from the respective ingots, and some small fragments of these variously treated, i.e., one has been heated, softened by heating, another has been heated and left to cool, and a third heated and quenched in water. The two kinds have been analysed by A. Dick and give- Without With manganese manganese added. added. Iron - 99-05 99-09 Manganese 0-03 0-10 Silicon 0-24 0-24 Sulphur -,0-05 0-07 412 Phosphorus - 0-02 0-02 Aluminium - 0-12 0-01 99-51 99.53 The carbon has not been estimated. See Percy's Metallurgy, Iron and Steel, p. 846. 3550. A series of specimens treated so as to show the effects on the fracture of steel of various ways of heating and cooling. These experiments were carried out by Col. H. Dyer, R.A., and the results communicated by him. No. 1 are samples of the forgings of steel which were used in the other experiments ; the fracture is finely granular. No. 2 have been heated in a cast-iron pan with sand to below the melting point of brass, which was secured by placing a pan with a piece of brass in the furnace along with the steel, and left to cool in the furnace all night, then covered in charcoal and swarf and left till cold ; the fracture is granular in the centre, but coarser round the circumference. No. 3 have been heated in smithy scale to a bright red heat, and left to cool in the furnace all night ; the fracture is much coarser. No. 4 have been heated in haematite ore to the melting point of copper. This is ascertained by placing a piece of copper on the hearth beside the steel, and when the copper melts the heat of the furnace is checked and made to cool as slowly as possible ; the steel casting being left in it. The fracture is moderately coarse. No. 5 have been heated in equal parts of haematite ore and sand to the melting point of copper, and left in the furnace all night to cool. Fracture moderately coarse, with a finer grained patch in the centre. No. 6 have been heated in iron swarf and charcoal to the melting point of brass, left to cool all night in the furnace, reheated to cherry red, cooled in water, and reheated to the melting point of brass (ascertained as in the case of copper), and left again in the furnace all night to cool. Fracture rather fine grained. No. 7 have been heated under the same conditions as No. 6, but have not been hardened. The fracture is coarser round the circumference and finer in the centre. No. 8 have been heated in lime to bright redness for 40 minutes in the furnace. The fracture is finely granular throughout. No. 9 have been heated in steel swarf and charcoal to bright redness 40 minutes in the furnace. The fracture is very fine grained. No. 10 have been heated in charcoal to the melting point of copper, and left in the furnace all night to cool. The fracture has a coarse ring round the circumference. No. 11 have been heated in iron swarf and charcoal to the melting point of copper, and left in the furnace all night to cool. The fracture is moderately granular. No. 12 have been heated in charcoal and steel swarf to the melting point of brass, and left in the furnace all night to cool. The fracture is pretty coarse. The points of all the specimens have been hardened in water. 3551. Steel coated with magnetic oxide of iron. By Bowers and BarfiV process, which consists of submitting the articles to be coated to super-heated steam, or to carbonic acid, or to petroleum vapour in a cast or wrought-iron chamber heated externally. By this means the surface is oxidized to a limited amount, producing a protective coat of magnetic oxide. See the various Patents, No. 862 of 413 1876, No. 2051 of 1877, No. 1280 of 1878, No. 3811 of 1880, and No. 3304 of 1881. Communicated by Mr. George Bower. 3552. Wrought-iron plate coated with magnetic oxide of iron by Bowers and Barffs' process, 1881. Communicated by Mr. Geo. Bower. See No. 3551. 3553. Wrought-iron pipe coated with oxide of iron by Bowers and Barffs' process, 1881. In this case the oxide is said to be the ferric and not the magnetic oxide. It has . a reddish tinge. . Communicated by Mr. Geo. Bower. See No. 3551. 3554. Large wrought-iron tube coated with magnetic oxide of iron by combination of Bower and Barffs' processes. Communicated by Mr. Geo. Bower. See No. 3551. SPECIAL ADAPTATIONS OF IRON AND STEEL TO VARIOUS USES. 3555. Three forms of manufacture of gun barrel. The first is a simple hollow tube. In the second a single bar is bent into a spiral, and the several adjacent coils are welded together into a single tube forming the barrel. In the third, three smaller bars are twisted into screws, and all welded together into a single flat bar, which is then itself twisted into a spiral to ibrm the gun barrel as before. 3556. Hollow hemisphere of mild steel. Manufactured at the Landore Siemens' Steel Company, at Landore, South Wales, and subjected to the dish-test cold, 1886. It consists of a piece of | boiler plate, dished cold. The tensile strain of this metal is 26-5 tons per square inch, and the elongation in 8 inches 28-5 per cent. 3557. Three bars of mild steel, tied cold, at the Steel Company of Scotland's Works, Glasgow. Manufactured by Siemens' process, 1885. The largest is about 1 inch in diameter ; the others are about inch and . They are tied into various knots and varnished. The follow- ing data have been determined in regard to the charge from which the material was taken. It contained : carbon, -17 per cent.; sul- phur, -05; phosphorus, -05; manganese, *47; and silicon, a trace. The steel has a tensile strength of 28-7 tons per square inch, an elongation of 30 per cent, in 8 inches, and an elastic limit of 14 '7 tons per square inch. Communicated by J. liiley. 3558. Plate of mild steel bent three times on itself, at the Steel Company of Scotland's Works, Glasgow, 1885. By Siemens' process. The steel of which this is made contains, carbon, 18 per cent. ; sulphur, -03; phosphorus, -04; manganese, -5; and silicon, a trace. Its tensile strength is 29 tons per square inch, the elongation was 24 per 414 cent, in 8 inches, and the elastic limit is 15 tons per square inch. Communicated by J. Riley. 3559. Bessemer mild steel boiler-plate, bent cold, and drilled cold from a f in. punched hole. Manufactured at the Locomotive Department, Crewe Works, 1877. Communicated by F. W. Webb. It is one of over 20,000 then made, proving how very uniform the material is. 3560. Three Bessemer mild steel plates, made for boiler and other purposes, two of which have been tested to their breaking point, at the Crewe Works. Communicated by F. W. Webb. This steel has a tensile strength of between 28 to 30 tons per square inch, and the elongation before fracture is shown by these specimens. The whole bars have elongated by comparison with the untested example about 1 inch. The breadth of the narrower part before testing is 2 inches. After separation is reduced by about 20 per cent. 3561. Four Bessemer mild steel angle irons, bent and folded cold, in various ways, at the Crewe Works.. Communicated by F. W. Webb. They are portions of: a steamer built for the London and Xorth-western Railway Company by Messrs. Lai i-d, of Glasgow, the material being made at Crewe. Not one of them shows the slightest sign of breaking. 3562. Bessemer mild steel rivet bars, bent cold at the Crewe Works. Communicated by F. W. Webb, 1877. 3563." Rough turning from Bessemer steel crank axles, for locomotives. From the Crewe Works, showing the homogeneity of the material. Communicated by F. W. Webb. 3564. Finished turnings from Bessemer steel crank axles. At the Crewe works. Communicated by F. W. Webb. 3565. Broad smooth steel turning, from the Woolwich Arsenal. Not tarnished by the moist air. 3566. Scale from rolling steel rail at Dowlais, South Wales. A thin sheet of dark sub-crystalline compound with cracked pyramidal elevations on the convex side. 3567. Seven specimens of iron for armour plates. Analysed for the Special Committee on Iron in 1863. They are stamped B 1, B 2, B 3, B 4, B 9, B 31, and P. 415 3568. Samples of armour plates which have been broken by shots. They are labelled W. and P. and show on the fracture a coarse crystalline structure with marked signs of lamination, brought about by the presence of mere or less slag, which has not been eliminated. 3569. A thick iron armour plate, which has been tested to the breaking point by Cammell & Co. of Sheffield. It shows a strongly marked fibrous structure parallel to the surface of the plate, with here and there brilliant patches, like the cleavage of surfaces of iron phosphide. 3570. Portion of Rodman's shot, fired at Shoeburyness. Rodman was the American who cast the, 70-ton gun in the Civil war in the United States. This has been analysed by W. J. Ward in 1868, and is found to contain graphite 2-83, combined carbon 0-34, silicon 0-82, sulphur 0-04, phosphorus 0-25, manganese 0-45 per cent, with a trace of copper. 3571." Portion of the Rodman shot, fired at Shoeburyness. Of granular grey cast iron, similar to that analysed. 3572. Piece of Dr. David Price's 15-inch shot, fired the 31st of March 1869. Communicated by Dr. Price. It is mottled cast iron, of not much purity. 3573. Piece of iron armour plate, smashed by a shot at Shoeburyness. It shows a highly laminated structure. 3574. Grey cast iron shot, broken up by firing against an iron target at Shoe~buryness. There are no signs of lamination in the fracture, which is finely crystalline granular to the surface. 3575. Piece of armour plate made at Portsmouth Dockyard and found to be bad. Communicated by Captain Drummond. It is very laminated and coarse, though thin, and shows much impurity. 3576. Specimen of iron broken by a shot at Shoeburyness, 1.866. Seen on one side the specimen has a beautifully silky fibrous frac- ture ; on the other side it is somewhat laminated, but highly crystalline ; at the cross section at the end the fibrous part breaks otf in black patches, and the rest shows a crystalline fracture. It thus appears that in the same iron it is different material, that has a fibrous or crystalline fracture. 416 3577. Two rivets destroyed by shot at Shoeburyness. One of these is broken across and shows its crystalline fracture, the other, originally identical in character, is sheared, and the surface of separation smoothed by some particles of iron being drawn along over others. 3578. Pointed end of an Armstrong shot which struck point blank an iron target at Shoeburyness in 1863. The shot was of grey pig-iron. This portion of it now consists of two conical masses, the smaller on one side, with the other one fitting over it, but turned out at the edges, like a piece of butter. Both one and the other are slickensided from the summit. This specimen demonstrates that under suitable circumstances solid pig-iron may be made to flow. This, however, is not generally the result. Much heat is usually developed by the impact, and a large quantity of the iron may be reduced to powder. The appearance of flame at the point of contact may be due to the fuming up of the highly heated iron dust thus produced. 3579. Piece of French screw torn out by a shot at Pole's Target, Shoeburyness, 1864. It shows for the most part a fibrous fracture. 3580. Piece of Armstrong gun breech - piece broken across. This shows a laminated crystalline fracture with bands of earthy matter running across it. Communicated by General Lefroy, of the Arsenal, Woolwich. A larger piece of the same breech is in the Royal Artillery Institution, Woolwich. 3581. Wrought-iron armour plate broken by a cannon ball at Shoeburyness. It shows a highly crystalline fracture, the length of the crystals being parallel to the surface, and they are mixed with much slag which is retained in welding one plate to another, in the usual process of manu facture. 3582. Iron from a piece of plate knocked out by a shot in Prussia in 1861. They are fragments showing a fibrous structure, perpendicular to the surfaces of the plate. 3583. Chilled cast-iron shot fired against an iron target at Shoeburyness and broken. It shows a radiating crystallisation passing to the surface as in white iron, but its colour is rather mottled. 3584. Fragment of armour plate tested at Shoeburyness in 1868, and which completely failed. It was made from an Armstrong coil, and split open by cutting, and then flatted out at a strong heat. The fracture is highly crystalline and 417 the plate is found to consist of oblique bands. Some of these are marked by a transverse fibration, and some by large plate-like crystals. It practically consists of a number of parallel bars welded together, and by re-heating the texture of the iron would become more largely crystalline. The thickness of the plate was 8 inches. Communicated by Gen. Lefroy. 3585. Part of a fly-wheel of an engine. From Dallam Iron Works, Warrington. Communicated by W. Flight. It shows a cavity into which octa- hedral crystals, single and combined, of iron project. 3586. Specimens of -f^ in. bolt iron, before and after re melting, to she w the effect on the fracture. The original bolt shows a finely fibrous fracture. A portion of the same has been melted, and the button when broken shows a very coarse crystalline and flaky fracture. Communicated by E. Riley. 3587. Section of a rail of Bessemer steel tested for the Great Northern Railway Company by Messrs. Cammell, at the Cyclops Steel and Iron Works, Sheffield, The weight of the rail is 80 Ibs. per yard, and it was tested by a weight of 1 ton falling on it from different heights, the distance of the points of support being 3 ft. When dropped from the height of 15 ft. the ton weight caused a deflection of If 'in. Ar the second blow, with a fall of 20 ft., the rail was deflected 2| in. At the third, with a fall of 25 ft., 4J- in. The bar was then reversed so that the deflected point was upwards. At the first blow of the ton falling from 15 ft. it deflected 3J in. At the second, with a fall of 25 ft., it broke. 3588. Collection of samples of rails made for the Great Kail way Company of Russia at the works of Terre Noire, Lyons, 1875. Communicated by the Terre Noire Iron Company. One is labelled as " Martin," another as " Bessemer," a third is laminated on the sur- face, and the other two are broken. Compare Percy's Metallurgy, Iron and Steel, p. 724. 3589. A section of one of these steel rails which have been tested by Chas. Cammell & Co., Sheffield, 1876. The chemical analysis shows the rail to have a large excess of phos- phorus. There is 0-15 per cent, combined carbon, 0-06 per cent, sulphur, 0-26 per cent, phosphorus, and 0-77 percent, manganese, with a trace of silicon. The rail sent to be tested was cut into three portions, each 4 ft. 6 in. long. These were rested on two supports with circular ends of 3 in. radius, the distance between the points of contact being in each case 3 ft. 8 in. Three trials were made rill the portions broke. A weight (of similar form to the support) of 2,240 Ibs. falling from a height of 15 ft. 4 in. broke it immediately. A weight of 1,232 Ibs. falling from 6 ft. deflected it ~ in., and falling from 8 ft. broke it. A weight of (505 Ibs. falling from 3 ft. bent the third piece T ? (r in., and U 61955. D D 418 falling from 4 ft. 6 in. bent it -/^ in., and from 6 ft. broke it. These results for a rail weighing 66| Ibs. per yard are not considered satis- factory. The fracture is remarkable as showing here and there brilliant white spots. 3590. Steel worked into the form of a tyre in section. Produced at the Lowmoor Iron Works, 1868. It has a moderately coarse crystalline fracture. 3591. Polished model section of a rail as used on the Bel- gian State Railways, 1887. Produced by the " Societe Cockerell," at Seraing, Belgium. Com- municated by C. P. Sandberg. 3592. Section of spoke of a cast steel wheel. Made at Monk Bridge, Leeds. Tested in 1885. It has a coarse crystalline fracture. 3593. Plate of iron which has been cast and which has round holes in it, punched cold, by the Carron Company, Fal- kirk, N.B. The plate contains an ornament in the centre consisting of a basket of flowers, and a frame which has been cast, but yet it has stood punch- ing cold without breaking. Communicated by Mr.-H. Blain, 1886. 3594. Tin plate made from No. 3 steel, equal to charcoal plate. The No. 3 steel was made at Blaenavon in a 3-cwt. Bessemer converter from pig-iron, containing 1 -4 per cent, of phosphorus. See the Thomas- Gilchrist process, Nos. 3440 et seq. 3595. Piece of sheet steel after cutting out the blanks for steel pen making. From W. Jessops & Co.'s Works, Brightside, Sheffield, 1885. It is returned from Birmingham to be remelted. 3596. Steel pens tipped with brass. Made at Birmingham, 1854. Communicated by Mr. Pershouse. 3597. Steel pens made from steel which has been smelted direct from the ore. They are stamped " King of Denmark." 3598. Cast iron used for plough-shares. From Fowler & Co.'s Steam Plough Works, Leeds, 1885. It is rast in chill from Weardale pig. The fracture is very finely granular, and shows grey iron in all but a narrow rim of white iron crystallising perpendicularly to the surface. 419 3599. Cast-iron screws annealed in coke dust. Made of Blaenavon iron at Mr. Walker's Works, Wolverhampton. 3600. Cast-iron screws made from Lorn iron, Ulverstone. They have been annealed for 48 hours in haematite, and have thereby lost weight. The iron will not mix with Blaenavon iron. Communicated by Mr. Walker. 3601. Iron nails in the shape of ornamental brass nails, ready to be electro-plated. Communicated by Mr. Fearn, electro-plater, Birmingham. 3602. Electrotype iron, produced in the process of s< AcieVage " at Messrs. Rollason's Works, Sheffield. Communicated by H. Bradbury. This is the deposit of 48 hours, and shows the pattern of a nature printed fern-frond. 3603. Piece of the iron column at Delhi. This column is between 40 ft. and 50 ft. in total length, and 26 ft. from the ground to the top, and 5 ft. in circumference. It is made of wrought iron, as shown by the small accompanying bar forged out of a piece. It does not sensibly harden by melting and cooling rapidly. Communicated by Lieutenant Cole. 3604. Iron coin issued by the Chinese Emperor in 1857. From the mint of Tuh Chow Foo, capital of the Province of Fuh Kien. It is a round coin with a square hole in the centre. It is black on the surface and badly cast. It was ill received by the people, and created great disturbance. Communicated by S. Birch, 1858. 3605. Iron tray coated with tortoise-shell lacquer. Made at Taganrog in Russia in 1865. Communicated by John Hughes, manager of the works. 3606. Seven samples of iron and steel wire which have been subjected to tests for tenacity by O. Schafer, 1886. No. 1 is a steel wire, with a breaking strain of about 120 tons per square inch. No. 2 is steel, whose breaking strain is 70 tons. No. 3 is steel, with a breaking strain of 120 tons. This is much thicker than No. 1, and as wires of the same quality have a less than proportionate breaking strain, as their diameter is greater, this must be of a different quality. No. 4 is of homogeneous metal, or soft iron, with a breaking strain of 30 tons per square inch. Nos. 5, 6, and 7 are iron wires of less tenacity. 3607. Collection of short lengths of fine steel wires which have been tested for tenacity, which is very high. They are tinned on the surface, and have been made the subject of elaborate experiments. A, B, C, D, and E, are all from the same rope. D D 2 420 Pieces from outside end of Coil. Pieces from inside end of Coil. Length tested 10 inches. Diam. in Inches. Per-cent- ageof Elonga- tion before Breaking. Breaking Strain. Diam. in Inches. Pcv-cent- ageof Elonga- tion before Breaking. Breaking Strain. Actual in Lbs. Calculated per Square Inch in Tons. Actual in Lbs. Calculated per Square Inch in Tons. 0195 1-4 113 168-9 0190 1-0 114 179'5 0195 1-0 101 151-0 0195 1-0 102 152-5 0195 1-0 101 151-0 01S5 1-2 97 161-1 0190 1-0 103 162-2 0200 1-2 113 160-6 0200 1-0 103 146-4 0195 1-0 97 145-0 0200 1-2 104 147-8 0195 1-2 102 152-5 B. C. 0190 1-0 103 162-2 0191 1-3 111 173-0 0190 0-8 95 149-6 0190 1-0 90 I4T7 0180 1-2 110 193-0 0188 1-0 93 149-6 -0190 1-0 90 141-7 0191 1-2 87 135-6 0190 1-0 103 162-2 0190 1-4 105 165-3 -0185 1-0 100 166-1 0186 1-3 104 170-9 D. E. 0181 1-2 100 155-8 0191 1-1 94 146-5 0192 1-3 110 169-6 0189 1-3 101 160-7 0192 1-4 110 169-6 0190 ro 95 149-6 0192 1-1 95 146-5 0188 1-4 111 178-5 0190 1-0 107 168-5 0189 1-3 104 165-5 0193 1-0 93 141-9 3608. Coil of thicker steel wire, tested for tensile strength which is very high. 421 This has also been tinned over, and has yielded the following results : Tests of bright Steel Wire. Length tested =10 inches. Diam. in Inches. Per-centage of Elonga- tion before Breaking. Breaking Strain. Actual in Lbs. Calculated in Tons per Square Inch. ^ 030 2-5 269 169-9 030 2-6 269 169-9 030 2-8 264 166-7 030 2-5 261 164-8 3609. Series of pianoforte steel wires, made according to Horsfall's patent. This paterxt was granted in 1854, and its essence consists in finally drawing the wire tempered at about dark blue, which is the melting point of lead, into which the steel wire is immersed. They are labelled Horsfall and Webster, Birmingham. Improved Vienna, No. 20, 103 grains; No. 14, 60 grains. One of these wires having a specific gravity of 7 '85 is said to have a tensile strength of 100-120 tons per square inch. Communicated by Dr. Pole. See Percy's Metallurgy, Iron and Steel, p. 854. 3610. " Fowler's Special " steel wire. Made by Rollason and Slater, Birmingham. Communicated by J. Fowler. In comparison with other wires this has the greatest breaking strain. Thus the crucible steel wire breaks with 40-60 tons per square inch. Patent steel wire with 80-90 tons. Plough quality ditto with 100-110 tons. Improved plough quality with 110-120 tons. This. requires 150 tons per square inch to break it. 3611. Wittenstrom's " Mitis " castings. Communicated by C. Wittenstrom of Stockholm, 1886. They consist of a double casting of a kind of bracket in the rough with adherent sand and some fragments to show its uniform and unblistered fracture. One of them is bent without breaking. 3612. Nordenfelt " Mitis " wrought-iron castings. Manu- factured in Sweden. Communicated by E. A. Cowper. There is a treble casting of a screw key, one of which is bent into a curve without breaking ; a screw key bent double three times, and another with one side polished ; and a shaped casting, one side of which is bent without breaking. These are from the same works as the last, Wittenstrom being the inventor. The process is the subject of a patent No. 8269, 1885. The principal feature is the addition of a small proportion of aluminium, which enables the gases to escape, and produces a uniform casting. See Percy's Presidential address to the Iron and Steel Institute, 1886. 422 3613. A hair-brush made of malleable cast iron, by Witten- strom's method of " Mitis " castings. The iron when treated in this way, i.e., by the addition of aluminium, is made to flow like milk, and runs down even with the small cavities represented by the wires. Communicated by J. Orum, 1887. One of the cones is bent in two, to show its flexibility. Watchmakers' Steel. 3614. Flat-spring wire for ordinary English watch. 3615. Two samples of hair-spring wire for marine chro- nometers. Both are white, polished, and flat, but one is broader than the other. 3616. Marine chronometer spring. This is the broader wire worked into a cylindrical spiral and tempered to a brilliant blue. 3617. Hair-spring for a small watch. An extremely small flat wire, wound into a flat spiral to which the flatness of the wire is perpendicular, and tempered to a brilliant blue. 3618. Main-spring of a watch of best construction. A broad band, wound into a flat spiral, and tempered to a purplish blue. 3619. Main-spring of an American keyless watch which broke suddenly. It is tempered brown and is broken about 1 inch from the centre. 3620. Spring of a lever watch made at Clerkenwell similar to those made for the Arctic Expedition, and which broke suddenly. It is tempered purplish brown and broke about 3J inches from the centre. 3621. Main-spring of a watch smaller than a threepenny piece. The exterior diameter of the compressed spring is about J inch, and the interior J inch, in the intervening ^ inch on each side are 8 coils. They are tempered a slightly purplish blue, except the inner one which gradually changes to white. 3622. Broken main-spring from a very large time-piece. A band J inch broad and tempered blue and purple, broken in several places. 3623. Minute steel parts of a watch. A horizontal escape wheel and cylinder and three small jewel setting springs and a screw. 423 3624. Chainwork for an English' watch. Made by women at Christchurch, Hants. These chains are composed of flat links, swollen transversely at each end, alternate links coming in contact and each rotating on a pivot passing through an internal link at the points where there are swellings of the external link. 3625. Series of watchmakers' small tools. They consist of one oblong file, double cut on the flat side and single cut on one narrow side, one square and one round double cut rat-tailed file, one minute single cut flat file, four half round files double-cut on the flat side only, and one flat bevelled file single cut on all the bevelled edges. They are all of foreign manufacture bearing the name of Proutat, Brizard, and Baumer, 3626. Watch pivot broach, or rimer. The smallest English one made. All the above specimens of steel used in the manufacture of watches (except No. 3619), were obtained from Mr. Brock of George Street, Dorset Square. 3627. Penknife with blades made of Wootz steel. The blades are stamped with the name " John Sellers and Son, Improved." Wootz is the name of Indian steel made by carburising compact iron. Its analysis is given in Percy's Metallurgy, Iron and Steel, p. 775. 3628. Penknife with blades made of Mushet's titanium steel. It is said also to contain tungsten. See No. 3511. 3629. Stirling's patent bell-metal alloy, cast into a bell. This is iron alloyed with a small proportion of tin. From the Exhibition of 1851. See Percy's Metallurgy, Iron and Steel, p. 162. 3630. Bell made of an alloy composed of 95 parts of white cast iron with 5 parts of antimony. The bell has two irregular holes on the top, bat the tone is good. 3631. Bell made of an alloy composed of 95 parts of white cast iron with 5 parts of tin. This has several irregular holes on the sides, and the tone is not very good. See Percy's Metallurgy, Iron and Steel, p. 162. 3632. Guard of Japanese sword hilt, made of iron overlaid with a pattern in gold. This has the appearance of being inlaid with gold, but it is not inlaid in the ordinary sense. The surface of the iron where the gold pattern is fixed is very finely cross hatched. Some form of stencil plate is apparently then used, which limits the gold to the pattern. Where it comes in contact with the iron it is pressed into the cross hatchings by which it is held in firm adherence. The pattern represents some imaginary bird in a bower. 424 DEFECTS IN IKON AND STEEL. 3633. Gun coil from Woolwich Arsenal showing the effects of the iron being " red short." The coarse fibres of the iron run parallel to the circumference of the coil, and on the outside they have parted in several places, making the sides jagged with chasms. 3834. Blistered boiler plate from the ventilation depart* ment, Houses of Parliament. 1881. The inner part has a great cavity, and is separated along the base of it from the outer part of the plate. It was found that the tube in this boiler had been made at another works, and not at Low moor as according to specification. 3635. Piece of a boiler plate which gave way along an arc of fracture 12 inches long. The rusty side of the specimen is the boundary of the crack. The fracture on the other side is silky-crystalline, and shows no signs of lamination. 3636. Part of a spoke of a cast-iron spoked car- wheel, which shows a hollow cavity in its interior. Made at the London Road Foundry, Edinburgh, 1881. Communi- cated by H. Louis. This is not a blow-bole or other ordinary defect, but depends on the metal, contraction occuring during solidification and thus causing the hollow. Often the interior of the cavity shows a more or less distinct crystallisation, and this seems to assist in the formation of cavities. The approximate composition of the iron is combined carbon 0-6, graphite 2-3 to 2-6, silicon 0-6 to 0-7, phosphorus 0-36, sulphur 0-08, manganese 0-4. 3637. Piece of the cast iron beam which broke at the Hartley Colliery accident, January 1862. The tensile strength was determined to be 473 Ibs. per square inch. The iron contains 2-68 per cent, of silicon, 1-11 per cent, of phos- phorus, and 0- 16 per cent, of sulphur. Communicated by Mr. Dunn. 3638. Piece of Bessemer steel, formed into an angle bar from the lower edge of the keel of the ship " Magdala," 1868, which broke on falling to the ground from the height of a few feet. Communicated by Sir Spencer Robinson. It has been analysed by W. J. Ward. Silicon - - 0-212 Manganese - ' - 0-382 Phosphorus - - . 0-067 Sulphur - 0-067 Iron - - 99-112 Carbon (by difference - 0-160 100-000 425 3639. {( Black plates " in the tinned plate process, which separate into two and rise into blisters. From the Cumbrian Iron Works, Newport, Mon. Communicated by 11. S. Roper, 1866. About 2^ cwt. of scrap taken from the blacksmith's shop was used up in the charcoal refiner's fire, and thus converted into stamp iron, mixed with the other iron, and made into several bars, and finally rolled into black plates with these blisters. 3640. Tin plates in which the tin leaves the surface of the iron and breaks up with a jagged edge. Due probably to the deposit on the surface of the plate of some slag which has not been sufficiently eliminated from the iron before tinning. Communicated by J. Williams. Pentyrch Forge, Cardiff, 1868. WEARING AND DECAY OF IRON. 3641. Tie rod of wrought iron taken from a cistern in Somerset House after 16 years use. The original diameter was J inch, and the service of water was inter- mittent. The tie rod is irregularly worn away, and shows longitudinal lines and knots like a stem of a tree, and in one part is reduced to about ^ inch in diameter. 3642. Pipe coated over with a crust of ferric oxide. No information accompanies this pipe. It is about 18 in. long and l inch diameter. Internally it is quite smooth and apparently unworn, but externally it is thickened up to 1 J inch diameter by a coat of ferric oxide (?), which is laminated and also split into longitudinal bands. 3643. Pipe for condensed steam from a battery at the Houses of Parliament, 1865. It is choked up to nearly the centre by a series of concentric deposits- of rust, which are additions to its substance and not derived from it, the pipe itself being almost entirely unacted on. 3644. Two halves of an iron steam pipe taken from the West Front smoke shaft in the Houses of Parliament after 3J years' use in 1865. This is the return pipe for the condensed water. It is about 1 inch in diameter. One half is very little altered, having only a deposit of rust ; the other half is deeply corroded and perforated in three separate spots, and thickened with rust elsewhere. These spots lie along the line where the tube has been joined, the joint having been cemented by a second metal (solder?). 3645. Scale from the interior of an iron vessel. . The thickness of plate which has decayed, according to the per- centage (63-53) of iron in the scale is 0-079 inch. The scale contains- ferric oxide 84 '24, ferrous oxide 5-87, water 7-80, and the outer surface contained oxide of lead in sensible quantities, and traces of chlorine and sulphuric acid. 426 3646. Broken boiler plates and bolts. No history. The plate has broken into laminae and also torn where the bolts were inserted. 3647. Stud belonging to a pump bucket, from Orange Street Waterworks, after three years' use. It was coated with Dr. Angus Smith's preparation before use, and has been continuously immersed in water during its three years' use. It is not very deeply corroded, but sufficiently so to bring out its laminated structure. 3648. Old and new back nut in the Range Boiler, Sealer's Room, West Front, Houses of Parliament. The old one had been in use about 12 months. The outside has rusted away to about one-half its original thickness. 3649. Round wrought-iron bar which had been for eight or nine years at the top of the front of a kitchen range. Communicated by J. H. Marshall, Edgbaston, 1875. This bar has never been redhot throughout, the side remote from the fire being always dark and it has been subjected to less heat than the lower bars but to a stronger draft. The bar was fixed in its place by a wrought-iron round pin let in at each end, one of which still remains. This would allow access of air to the interior. In any case the ends have oxidised along the fibres more than the centre has, which has caused expansion and thus produced the separation and bulging at the ends. 3650. Altered steel bar from a furnace bottom. Communicated by R. Pearce, of the Black Hawk Silver and Gold Smelting Works, Colorado, 1878. Part of the bar is imbedded in con- solidated cinder, the consolidation being due to the iron derived from the bar. The bar itself, both in the imbedded portion and the other, shows a concentric structure, a hollow centre and sheaths of scoriaceous matter which are only partly metallic, so that the whole bar is chemically altered and has become of smaller specific gravity. Its diameter is about l inches. 3651. Decayed half-inch cast-iron plate forming part of the interior tubbing of the upcast shaft of Monkwearmouth Colliery, Sunderland. It was placed in position at a depth of 180 fathoms from the surface iu 1863 and taken up in 1871. It is now entirely turned to rust which is so lightly aggregated that it is like a sponge with a very low specific gravity. Communicated by Lieut. Cundall, R.A. 3652. Scale scraped off the surface of a " Con way tube." From an area of 2 ft. 4 ins. by 1 ft. 9 ins. Communicated by the London and North-western Railway Company. Analysed by R. Smith, 1869. 3653. Scale rubbed off the surface of a " Conway tube." From an area of 24 ft. 4 ins. by 1 ft. 9 ins. Communicated by the London and North-western Railway Company. Analysed by R. Smith, 1869. 427 3654. Altered cast-iron case of the condenser of H.M.S. " Spartan." From the dockyard at Sheerness. The condenser tubes were of copper and the case within which they were contained was of cast iron. The copper tubes carried steain within and between them and the case sea water circulated. The fragments of the case are nearly or entirely converted with a porous ferric oxide of light specific gravity in the bulk. 3655. Part of an old cast-iron water pipe which had been in use for about 8 or 10 years, at Llanelly, 1863. It is of unequal thicknesses on the two sides, but has not been sensibly corroded in this part, but shows the spots to which concretions have been attached. 3656. Concretions of hydrous ferric oxide which have formed inside the above pipe to the extent of choking it up. They are irregular soft brown lumps, showing concentric structure, and on heating them to 110-120 C. they lose 5-90 per cent, of weight. There is no evidence that they were derived from manufactured iron. 3657. Mass which is supposed to have been an iron rod embedded in scoria from a charcoal furnace of a steel works at the Brades. It is now a light porous grey material containing glittering particles and unlike either graphite or any compound of iron. 3658. Two rivets from a boiler which exploded at Messrs. Hickman's Works, Staffordshire, in 1856. On one of these is seen anhydrous, and on the other hydrous ferric oxide, the former from above and the latter from below the water line, indicating that above the water line the boiler had been red hot. 3659. Old cannon ball which has fallen amongst shells and gravel below the sea level. The cannon ball, about 3 inches in diameter, is partly converted into hydrous ferric oxide, the surface being swollen in parts and divided by irregular cracks, it is surrounded by a dense coat of the same, and beyond this is formed a conglomerate of shells and stones agglutinated by the same hydrous ferric oxide derived by solution from the ball. 3660. Cannon ball exposed for a long period to the action of water by which it has been oxidised and lost its shape, being corroded on one side. 3661. Hook and shackle of coal pit tub left in water for 25 years. At one of the pits of the Staveley Coal and Iron Company, near Chesterfield, a fire occurred about 1857, and water from the canal was turned in to put it out. The old workings in some parts of this pit have been filled with water for upwards of 25 years. On reopening these levels two trains of pit tubs were found in them ; the woodwork was 428 perfectly sound, but the iron was converted into oxide ns seen. The Jinks are now all cemented into a mass, which consists entirely of hydrous ferric oxide, which is porous, arranged in concentric bands within, and raised into irregular knots oa the surface. Communicated by Mr. Markham 1887. 3662. A key which has lain for some time in the bed of the Thames. It is coated over with a conglomerate of stones and shells, which are fixed by the impregnated ferric oxide derived from the decay of the key. Communicated by W. Cutter. 3663. Smith's hammer which has been for a long time buried in swampy ground. Found in making an extension of the Metropolitan Railway Carriage and Waggon Works at Saltley, Birmingham, in 1876. The wood of the handle is unaltered, but the iron head shows the running of the fibres of the iron, both in the body and round the head ; they are brought out by weathering. Communicated by F. W. Marshall. 3664. Piece of an old cannon ball taken out of Falmouth Harbour. It is now loose, porous, crumbling dust of hydrous ferric oxide, with some bright metallic particles scattered irregularly through it. 3665. Rust scaled from the horizontal part of house railings in Lincoln's Inn Fields. It shows a thickness of at least half an inch, and is highly laminated either after the structure of the original part, or by intermittent formation. 3666. Piece of an old iron gun raised from beneath the sea at Tenby in 1856. This is changed into a compact black oxide, not at all soft, but brittle under a blow ; it shows no concentric or parallel structure. 3667. An old cast-iron shot from a ship at Chatham Dock- yard. The external surface has become oxidised, and a thickness of about J inch has mostly pealed off, leaving an irregular core with depressions all over it. Communicated by Col. Pasley. 3668. Old wrought -iron bars out of a dismantled ship, Chatham Dockyard. One end has in both cases split open, and decayed in laminae, and one has a conglomerate of gravel formed on it. There was a large quantity of broken scale detached. Communicated by Col. Pasley. 3669. Part of the breach of a cannon showing the touch- hole and tube after firing 530 rounds. 281 rounds have been fired with a 12 IDS. charge, and 249 rounds with an 11 Ibs. charge. The tube is eroded in a very irregular way. 429 3670. Section of old rail after use for 29 years on the Church Fenton and Harrogate line of the North-eastern Railway. When laid down in 1847 it weighed 65 Ibs. per yard, and when taken up again in 1876 it weighed 61 Ibs. per yard, but its section shows not the slightest truce of developed lamination. Communicated by T. Harrison. 3671. Section of old single head rail used by the North- eastern Railway Company. It is a Welsh rail with Crown stamped on it ; it originally weighed 65 Ibs. to the yard. These rails were laid on the Newcastle and Berwick section on the down main line between Scremerston and Tweedmouth in 1846, and were in use there till 1863. They were then taken out and laid in a siding at Scremerston Lime Works, till they were finally taken out in 1873. They have worn well. Communicated by T. Harrison. 3672. Section of old double head rail used by the North- eastern Railway Company. It is a Snowdon and Hopkins' rail, weighing 66 Ibs. to the yard. The rails were laid on the Kelso branch up line between Velvet Hall and Norham in 1S57, and were in use up to 1876, all having been turned but none replaced. They show vertical divisions by intermixed impurities. Communicated by T. Harrison. 3673. Section of old single head rail used by the North- eastern Railway Company. It is a Hudson rail, weighing S3 Ibs. to the yard. These rails were laid on the Berwick Bridge in 1849, and were taken up in 1867 and laid on the Kelso branch down line between Kelso and Spronston, and were still in use in 1876. < 3674. Section of old double head case-hardened rail used by the North-eastern Railway Company. Il is a Derwent and Consett Iron Company's rail, weighing 82 Ibs. to the yard. These rails were laid on the Newcastle and Berwick section near Chevington station on the up line in 1860, and were still in use in 1876. The rails were case-hardened by the North-eastern Railway Company. The rail has now been reduced to 79-J Ibs. per yard, or a loss of 2 Ibs. in 14^ years. 3675. Specimens illustrating the unintentional welding together of two steel surfaces. The part with the thicker stem was originally separate from the other, the two being placed together along the surface indicated bv the line beyond the collar. They have become welded into one piece so firmly that it has been easier to break the substance of the steel itself than to part them. In a large lathe for turning a special class of work rotation is given to the work by means of a cross shaft. The end of this cross shaft is provided with a flat-ended steel plug (one of the pieces here welded together), which bears into a similar plug (the other 430 piece), rigidly fixed to the frame of the lathe but capable of adjustment. The two steel surfaces are kept in contact, and are made as hard as possible, and are specially provided with an arrangement to keep up the supply of oil. Nevertheless, three or four times during 15 years they have welded together by the hent of friction produced by the rotation. Communicated by J. Taylor, 1880. 3676. Piece of a cast-iron tomb plate erected in Wadhurst churchyard, Sussex, 1613. It has a superficial coat only of oxide, within it is still solid white iron, proba,bly of Sussex origin. 3677. Piece of an old iron slab from a grave in Em-wash churchyard, dating from the 14th century. This is a portion of the slab mentioned by M. A. Lower in his paper on the Iron Works of the South (Contributions to Literature, p. 97), and figured in Boutell's Christian Monuments. It is certainly cast iron, and, according to antiquarians, there is little doubt of its being 14th century. Communicated by A. Nesbitt. 3678. Ilusted iron from an ancient cemetery at Hallstadt, in Austria. It is rusted to the centre, so that its original nature cannot be ascertained. Communicated by J. Evans. 3679. Portion of one of the iron clamps from the Parthenon at Athens. This shows a clean blue-white granular crystalline fracture as of wrought iron. Communicated by J. Evans. MISCELLANEOUS. 3680. Timber from an old tree, found 36 feef below coping level of New Basins, or 30 feet below Trinity high-water mark. From the Admiralty Works, Chatham. It is perfectly sound. For comparison with iron decayed under similar circumstances. 3681. Wood from a bed of peat at Barking in the sewage tunnel to the Maplin sands. Some 20 or 30 trees seen in situ, in 1866. 3682. Two examples of Irish bog oak in its less altered condition. Communicated by J. Hawkshaw. 3683. Charcoal which has been heated to a high tempera- ture for several hours. 3684. Charcoal from sugar which has been heated to a high temperature. 431 3685. Finely divided graphite prepared by Sir Benjamin Brodie's process. Communicated by Sir B. Brodie. 3686. Anthracite particles collected round the top of a blast furnace at Ystalyfera, near Swansea, Glamorganshire. The furnace was let down and the blast kept on. In this way the coal is carbonised but has no ore to reduce. 3687. Coke formed where gas leaked from a gas retort, Stafford Gas \Vorks. (1847.) The same mammillated forms in one specimen and some coarse hair- like processes in the other are shown, and are referred to the decompo- sition of gas by the heat. Communicated by Mr. Clift. 3688. Coke-like mass from a gas retort, showing mam- millated surfaces. 3689. Specimens illustrating the effect of carbon in fusion. Two pieces of platinum foil have been exposed to a high temperature in small Stourbridge clay pots. One of them was imbedded in fine white sand, and in this case the platinum was untouched by the heat. The other was mixed with carbon, and globules of silicide of platinum have been formed by the extraction of the oxygen of the sand by the reducing action of the carbon. 3690. Specimens of devitrification of glass, illustrating the formation and colouration of slags. See Percy's Metallurgy, Fuel, &c., p. 33. These consist of A. Three specimens produced during the rapid cooling of sheet glass. These show mere specks scattered throughout the glass. They were produced in the pot of a gas furnace that was cooled as rapidly as possible. B. Two specimens produced during the slow cooling of sheet glass. These show large nodules 5 or 6 inches in diameter, impinging on each other. They were formed in a furnace that was kept about the melting point of the glass for 10 days and then allowed to die out. The crystal- lisation has spread from the surface and sides along the bottom of the pot, the central portions of the glass being the last to crystallise. C. A darker glass with nodules about ^ inch diameter from the " pockets " of a gas furnace. D. " Ambitty " glass. Obtained from the furnace before the pots are quite worked out. All the above are full green in tint. E. A specimen consisting of glass of two colours separated by a band of devitrified glass ; the one is full green, and contains numerous devitri- fication centres ; the other is blue-green, and contains none. The com- position of this sheet glass is, approximately, silica 73 per cent., soda 13 per cent., lime 13 per cent., and alumina and ferric oxide 1 per cent. The specific gravity of the devitrified portion is 2 5823, or a little less than that of the glass, which is 2-5919. 432 F. Results of experiments on the devitrified glass. The material A N 69 was placed in fragments in a crucible in a large Siemens' furnace. At the end of 12 minutes (in which time fragments of the glassy portion treated similarly had completely melted) it was in a pasty state, giving a fibrous silky appearance on proof B N 69. In 88 minutes more it was entirely converted into the vitreous form, but was full of bubbles. C N 69. (Compare the statement on page 33 of Percy's Metallurgy. Fuel, &c.) G. The specimen marked A N 61 is formed from vitreous glass of specific gravity 2-5398, by keeping it for 144 hours at a bright red heat and surrounded by sand. It has a specific gravity of 2-4955. H. Photograph of an hexagonal crystalline plate forming in glass during the process of devitrification, magnified 63 diameters. All com- municated by W. D. Herman, St. Anns Glass Works, St. Helens, Lancashire, 1872-3. 3691. Box containing some results of Sir James Hall's ex- periments on the effects of heat and compression. These specimens belonged to Faraday, and are labelled by him. Communicated by his widow. They comprise A. A specimen of Rowley Rag, accompanied by another specimen of the same which has been melted and then allowed to slowly cool, bj'' which means it has returned again to a crystalline form. The specimen is partly composed of the pot in which it Las been fused. B. A glass tube with the following label " Two specimens in one " experiment of the effects of H[eat] and Compression], The uuder- " most (next the wooden cup) was a piece of common chalk. The other " (if I am not much mistaken) purified by Mr. Hatchett. They were " both in tubes of platinum, which metal was fused by the intrusion of " the fusible metal. The upper specimen, where it has been by that " means brought into contact with the porcelain, has run much." C. " Some results of carbonate of lime exposed to H[eat] and " Compression]." D. "Compound of silex with carbonate of lime obtained by H[eat] " and Compression]." E. " Chalk turned into a substance like marble by H[eat] and " Compression]." F. " Pounded limestone formed into stone by H[eat] and " Compression]. An old. experiment made in 1799." G. " Common coal melted under compression retaining its power of " giving flame." H. "Piece of wood fused under H[eat] and C[ompression], and re- " taining its power of giving flame." 3692. Samples of Wedgwood's pyrometer. Made by the original inventor, Josiah Wedgwood. Each is stamped with the figure 2. 3693. Specimens illustrating the power of Welch's small Wast furnace. A mass of malleable iron melted in a small Stourbridge clay crucible. The iron shows a very remarkable smooth concave fracture. Commu- nicated by Mr. Welch. 433 3694. Box containing samples of malleable iron which have been melted in Welch's small blast furnace. In this furnace four ounces of iron are melted in 18 to 20 minutes. The surface of these specimens has been polished with tin oxide, but are otherwise untouched and as they left the crucible. They were ob- tained by melting iron filings with pure ferric oxide, covered with pounded glass. Communicated by Mr. Welch. 3695. Round balls of ferruginous concretions produced from the water in the lead tanks of the Wortley Silkstone Colliery. Described by Thomas Andrews to the British Association, 1879, and communicated by him. The water which produces these percolates through the coal strata for 35 yards into a bed of silkstone coal, whence it is pumped up. It always has an acid reaction. It deposits 2-45 grains per gallon on boiling, and it contains in the same quantity 18-16 grains of calcium sulphate, 19-52 grains magnesium sulphate, 1-03 grains potassium chloride, 7 '34 grains sodium chloride, and 8-27 grains sodium sulphate. When this water is not previously precipitated but passed direct into the lead tank, at the end of two or three weeks these balls are found, the ironwork of the colliery engine or boilers being at the same time corroded both by the water and the steam generated from it. The water is kept at a temperature varying from 140 F. to 188 F. by steam playing on its surface. The balls have a concentric structure, and the general aspect of hydrous ferric oxide. The analysis gives Moisture - 2-30 Loss on ignition - -24-40 Silica - 1-80 Ferric oxide - - - 62-86 Alumina - 5-43 Phosphoric acid - 2-81 Lime - 0-40 100-00 3696. Boiler incrustation of gypsum. Characteristic crystals formed in the boiler of the Chyandour Works, North Crofty, Camborne. Communicated by A. K. Barnett. 3697. Specimen illustrating the formation of iron pyrites by solution. A fragment from a log of wood belonging to the yacht " Osborne " in 1872, in which crystals of iron pyrites may be seen along a flaw. This log had lain for a considerable time in a timber pond at Ports- mouth, into which two drains discharged. Communicated by W. Weston. 3698. Crystalline mass of green vitriol. From the 40 fathom level, Duchy Pern, Newly East, Cornwall. Communicated by Mr. Peto. Produced by the atmospheric decompo- sition of pyrites, and covered with small excrescences of fibrous crystals of an allied species. U 61955. E E 434 3699. Mass of sulphide of iron which ran down in the form of a stalactite outside a bisulphide of carbon retort. Communicated by W. Ratcliffe. The colour of the sulphide indicates the presence of some ferric oxide, which is not usual in the ordinary commercial product. 3700. Stalactitic mass of oxide of iron ; locality unknown. It is broken across, and each drop shows radiate crystallisation. 3701. Crystalline slag produced in carrying out " Hollo- way's process." It is a silicate of iron, made by blowing protosulphide in a gannister- lined converter, and when all had been oxidised, teeming into a ladle, and allowing it to set. It is a black mass, with thin brilliant rectangular plates standing up in the hollows. 3702. Another block of the same character and origin, showing the irregular shape of the cavities. 3703. A similar specimen, with many of the crystals seen on the flat side. 3704. Slag obtained in the carrying out of the " Holloway process." This is obtained by exposing tap-cinder to a high temperature with lime, and then pouring it out. It is a failure in the process. It is a minutely scoriaceous mass in which large plate-like black crystals are abundantly formed ; the plates being composed of innumerable smaller ones, which are placed edge to edge. 3705. Spence's patent metal formed into a casting. This material was introduced in 1880. It is made by fusing together a mixture of finely pulverized metallic sulphides, with varying pro- portions of sulphur. It expands on cooling, thus being specially suit- able for casting. It melts at about 320 Fahr. It is very little attacked by acids, and is unaltered in the atmosphere. It is thus adapted for various kinds of fastening. 3706. Compounds of an unspecified alloy with various metals. A. contains 90 parts of the alloy to 10 parts of gold, the total weight being 98 grains. B. contains 90 parts of the alloy to 10 parts of silver. C. contains 50 grains of alloy to 50 grains of silver, the total weighing 99J grains. D. contains 50 grains of the alloy to 50 grains of allumi- nium. E. contains 90 parts of the alloy to 10 of tin. 3707. Bellows for a continuous blast as used in Orissa, Lower Bengal. It consists of two hemispheres of hard wood side by side, rudely hollowed and each connected with a projecting hollow tube, the tubes on the two sides being carried parallel to each as far as the end of the bellows ; the whole is cut out of a single piece of wood. The hollow of the hemispheres is covered with a piece of buffalo hide, with a small 435 piece of string tying it to the end of a bent bamboo fixed into the ground close by. The method of action is as follows : the bamboo acts as a spring, drawing up the string, and with it the leather cover of the bellows to its utmost stretch, while air enters through the central hole. When the hemisphere is thus filled a man places his foot on the hide, closing the central hole with his heel, and throwing the whole weight of his body on to that foot, he depresses the hide, and drives the air out through the tube, while he depresses the bamboo with his hand. This operation being done alternately on the two sides produces a continuous blast. See Percy's Metallurgy, Iron and Steel, p. 261, the description being written by Mr. H. F. Blandford. 3708. Pair of circular bellows used in native smelting. These consist each of a circular block of wood, enlarging towards the top. The upper side is hollowed out for about J the depth, and the solid block below is perforated obliquely. The hollow at the top is covered with strong buffalo hide, with a hole in the centre, and tied over a rim at the circumference. These, with a tube fixed into the holes at the bottom and used together, would act in the same way as the last. Locality unknown. 3709. Large conical leather bellows used in native smelting. At the small end it is fixed to a large but short copper tube of conical shape, at the large end the two sides are sewn tightly to two rods of split bamboo, which at one end are tied together loosely enough to serve as a hinge, and at the other are produced beyond the bellows to serve as a handle, but they can only be separated to about 15, and the whole bellows then open at the base. It is not obvious how they act. Locality unknown. I UNIVERSITY OF CALIFORNIA LIBRARY BERKELEY '** Return to desk from which borrowed. : <^; . This book is DUE on the last date stamped below. JUN4 USBARY Ut NOV 2 1/1 : ONl-V 1988 UEPT. LD 21-95w-ll,'50(2877sl6)476 lU U.C. BERKELEY LIBRARIES BODllbllflM 8/-L UNIVERSITY OF CALIFORNIA LIBRARY