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Thosa too iarga to ba antiraly included in ona axposura ara filmad baginning in tha uppar iaft hand corner, left to right and top to bottom, as many f ramus as required. The following diagrams illustrate the method: Les cartes, plenches. tebleaux. etc., peuvent Atre fiimte A des teux de reduction diffirenti. Lorsqus 's document est trop grand pour Atre reproduit en un seul clichA. 11 est filmA A partir de I'angle supArieur gauche, de gauche A droite. et de haut en bas. en prenant le nombre d'images nAcessaire. Les diegremmes suiventt illustrsnt la mAthode. rata 9 •elure, A 3 I2X 1 2 3 1 2 3 4 5 6 ^mf^ ff THE •*«!«*■* rPTiil V ''i»''-. ONTARIO, CANADA, I'.V R. P. ROTHWf-:LL, M.H., NIW YDKK ( I lY. A Paper Rfad bf.forf. thf Amfkican Institute of Mining Engineers, at the Phii adei.phia Meeting, February, 1881. AUTHOR'S EDITION. 1881. 1^ r r^ . .'I c^ Wufmit^y t^d^fv^ ^o/um/ti{ V/r i i THE GOLD-BE AlilNG MISPTCKEL VEINS OF MARMORA, ONTARIO. CANADA. BY R. P. ROTH WELL, M.E., NEW YORK CITY. About thirty miles north of the city of Belleville (which is situ- ated on a branch of Lake Ontario), and in the township of Marmora, Ontario, th' 'e is found a belt of f;old-l)earin<^ quartz veins which present geold. 'cal, mineralojjical, and econoniie features of };;reat in- terest to the piwfi'ssion. The district in which these veins are found is characterized as a rolling; country, with low rounded hills of syen- itic granite, overlain on the flatdvs of the hills by Silurian limestones, which lie in nearly horizontal beds, and in some pla<'es are so fine in texture as to afford lithowra]ihic stone of a fair (piality. The jjold-bearing veins run north and south through this belt of syenitic granite, and are qnartz-*^lled true fissures, with micaceous or talcoid slates forming the wmIIs (»f and horses in the veins. This talcose, slaty rock is evidently the product of the chemical decom- pofiiti(m of the syenite along the fissures, the quartz being segregated from the country rock into the veins, and the hornblende of the syenite furnishing the magnesia of the talcoid slates. The veins, besides quartz, contain also, as gangue, crystallized calc-spar, and occasionally crystallized black mica. The ore scattered through this gangue, in heavy bands in some places and in detached, well-formed crystals at others points, is an arsenical sulphuret of iron (mispickel), having a composition of about 55 per i-.n. of ir^a unO cr cent, of arsenic, and |)erhaps 20 per cent, of sulphur. Th." ispickel contains the greater part of the gold for which the mines worked, but free gold is also found scattered through the quartz in si lall leaves and grains, and it is also found, showing freely at timves, in the mispickel itself. The tests which have been made of these veins and their ores have so thoroughly established the facts of the continuity of the veins, both in length and depth and the economic value of the ores, that (JOlil)-HKAKlXO MIHl'lCKKI. VEINS OF MAKMOHA. the interest which would naturally he tak^n in h«> |»romisinf; a pros- jKH't as this was, (!ven hcCortMlfvelopnient, has now ihrpciuMl into the substantial form of an interest in a ^^reat inOustrial entcr|»ris('. ( Jol(l«\vas (irst (lis(;(>v«'re«l in this distrirt in 1 8(5') as tree jjoM in <|uart/ :i!:radj(' attempts have since hecii made at two or ihret! points to treat the ores, chicHv hv raw amalirau'ation. As mifrht have been anticipated from the nature of the ore, hut a very small proportion of the jrold was saved in this way, whih' th(^ expense <»(' treatment in the small and primitive niills adopted was jjreat and the loss of (piicksilver heavy. There was neither experi- ence nor technical knowledge available at tin; time, and no sufUcient capital to put up suitable works or todeveloj) tin' mines ; hente they have lain iille all these years without a sinj^le serious effort to work them on an economical bu is. Xevertheless, many tests (»f the ores were made, some on (piite an extensive scale, in reduction works in the United States and England, and the result** were invarial)ly highly satisfactory. liy far the most extensive and the only systematic tests of these veins and their ores have been made upon the properties shown in the acconi|)anying maps, and which form a portion of the properties combined under the ownership of the Canada (/onsolidated Gohl Mining Company. From these tests some four or five parallel veins have lu'cn proven to «'xist in a belt of AOO or 600 feet in widtii, running through t'le property of this company fora length of over three-tjuarters of a mile, while the main vein has been opeuitl on adjoining properties, making a total proven length of this great fissure (»f about three miles on the vein, a fiiet which, next to actual sinking, may be considered the best proof of the continuance in depth of the veins. Three of these veir.s have been proven on this property by cos tea n pits an l/i to lAO feet. In this manner, the east or main vein has been thorcuighly explored gyer a length of alK)nt 800 feet by shafts of from 4(Ko 150 feet in deptii ; these have, in every ease, l)een in pay-ore all the way; their lowest points are now in as gooil ore as has l)een found on the property ; and they have shown this vein to have a thickness exceed- ing 20 feet in many places, and averaging probably 8 or 10 feet; while the middle and west veins, though smaller, have still appar- ently u thit^kness of three feet ant! upward. As each foot of thick- ness for a length of 700 feet anI,l»-HKAHrN(l MIHIMCKKI, VKINS OF MAIIMOHA. in tlilH mnall part of tlii?< vriu aloiw, li in <;(I,(M)(» t.» 7o,()stion of greatest interest is the average gold eon- tentM of the ore; and as this has been determined in a very thorough manner under my own supervision, 1 shall enter somewhat into the detail of the worU, as showing what is eonsidereJ».47 per ton. Professor E. J. Chapman, of the l>niversity C-ollege, Toront(), savs : " 1 have made assavs of its ores fn)m time to tiuje, and I have never till leickel, erushe.48; silver, §15.71. Total, STOJMU. G all ht|ii('kel, Di'iliK't I ton for irimsjii" in Imlk, Iciivini; " } ton for inlVrior inispiclu'l, li-uvin;; " for loss in reduction $7 23, Icivinj;. Or not yield of oro in treatment §30 per ton $372 29 74 48 37 23 30 00 F. VV. Dahne, Fscj., who dressed a lot ofthis(»re sent to Swansea, says: "The ore I treated eontained, heforedressin*;, 2^ ounces of gold to the ton (2240 poui Captain lienjamin .^ .i. ..mer,whoexamined these mines tor .Messrs. John Taylor & Sons, of London, carefully sampled the ores from the different openings, and had his samples assayed hy Professor Chap- man, of University College, Toronto, who obtained the following as the average of a number of assays, gold eountetl at §20.GG per ounce troy: Sample No. 19, Gold $38.r.5 jx-r ton of 2000 pounds. " No. E, '• 24.87 " No. F, " 30.00 " " " No. O, " 24.74 Average, S31.21. The amount of silver in these samples never exceeded \ ounce per ton. TESTS ON A LARGER SCALE. Two barrels of average ore treated at Balbach's works, in Newark, N. J., yielded : From Bad Vein — Gold, §23.76 ; silver, §4.07. Total, §27.83 per ton of 2000 jwunds. From O'Neil ISha/t— Gold, §25.02 ; silver, §4.39. Total, §30.01 per ton. Four barrels of ore seut to Messrs. Richardson & Co., Swansea, A OOLD-HEAKINO MWPK'KEL VEIN8 OF MARMORA. f^ . yielded uh follows (iwsuys beinj^ reduced to dollars per ton of 2000 pounds): Tuttie ^haft.—iU>U\, 1^93; silver, $7 per ton (2000 pounds). Gatling CompanifH Deep iShdJt. — Gold, l?.'J7.2l ; silver, $20 per ton (2000 |K)und»). (iatlhuf Coiaiomids). (kitlinr/ Company*n (/Neil -S7«t/?.— Gold, $23.16; silver, $100 per ton (2000 j ounds). The report lor a large lot of ore from the O'Neil shall, sub- sequently sent l.o the same Swansea parties, was as follows : For 19.8 tens: Gold, $23.15; silver, $0.50 per ton of 2000 pounds. For 9.9 ton« : Gold, $27.90 ; silver, $0.75 per ton of 2000 pounds. For 4.4. tons : Gold, $55.H1 ; silver, $0.50 per ton of 2000 pounds. Analyses of pure mispiekel, made by Thonia.** Thomas and J. Hernaman James, Assayers in Swansea, to Messrs. Richardson & Co., were as follows (the gold being reducetl to dollars in a ton of 2000 pounds at $20.67 per ounce) : Peroxide of iron Silleu ! Sulplnir I Arst'iiic Nickel 1 Silver (jMjr ton of JOiKi poiiiuls). 1 Gold ((ler ton of JJOij poniKlH)... SMAl.l. LARUE CRYHTAL1.IZATI0N. CKVHTALLIZATIO.N. W.0O .)»).(X) 0.51 ().(i:t 19.03 i«.i;) •J5.70 •j;i.o.i«,5 1 Mr. K. W. Harmon, in 1876, ttisted the ores from these proper- ties in the interest of Boston parties, who had a patent process for treating sulphuret ores. The following are the results obtained by Mr. Harmon from average samples selected by him.self : Per ton of iOOO |M>uudi). io 1. Ku»t Vein Uatl ng Company, gold, . $128 84 2. II II II 87 84 3. II <« II 87 84 4. II It II 76 68 6. Middle Vein II ti 48 Ifi G. II II II . 116 96 7. West Vein II II 41 28 8. II II « , 120 40 9. Sample from all of foregoing, . » 61 92 8 (H)LI>-BEARISr; MLSPMKKr. VKINS OF MARMORA. No. 10. GatlirK ^HHitb 41 28 "11. " five ■ere', 550 40 " 12. " " 595 12 «' 13. " *• ....... 37 M " 14. Williams min<>, tailing)*, ... . 84 40 ••15 (iatlingCom|i«ny— Shiift, fm' jijoM, . . 440 32 •' IC. (iatlinjj r.>ay.s of lots of from two to three tons viich : ' Ore. Tiillings. No. 1, $30 '.»0 $30 30 "2, 41 20 6 67 "3, «6 23 6 87 "4, ... ... 41 20 6 87 •'5, 51 50 8 58 •• (J, 44 71 12 04 Average g<»ld in 1».7 tuns was ^85.46 per ton, counting gold at $20 per ounce. Gold actually save(' his a.s.say.s wiis iw follows: I)c»'p sliiifl, liottotn, N. level S. level, .... A shnft (3 >nniiiling.'»), . Tuttle shuft, .... AverHge after purtinsj; gold, . $*2I.'>0 |ier ton. (i.tJO '• 7.50 •• ]"< U-2 '« l.TOC, " By far (he mo.«»t exhaustive tests (»f these ores were made under my own direetiou. Having seeured a working bond tipou these propertie.s, I carried on mining and milling operations with a force of eighty or ninety men during nc^arly four months. During thi.s time, seven shafts were worked upon and attained depths ()f from forty to one hundrtKl and ten feet ; and two levels v»f forty feet each iu length were driven. Three of the.se .shafts, namely, the Tuttle, the A shall, the deep shafi, and two levels were tho.se upon which tlu; mo.st work was })erformed, and it is to the ore from the.se that the following remarks are confined. These openings prove a length along the main vein of about .seven hundred feet, as may be seen by reference to the accompanying map.s. The ore extra(!ted, vnihoni any ftortiut/ irhatevrr, was taken to the mill ; it wa.s then weighed ann(^ hundred and eight lots, nearly all representing five tons of ore, were assayed separately, while fifty-one tons from the Tuttle shaft were sampled iu the same ciireful mamier in one lot by Mr. Tluunatj Macfarlane, of the Wyandotte Silver Smelting Company. The assays of these several samples are given in the following table. It will be noted that the richer five-ton lots were obtained by selecting the heavier sulphurets from the remainder of the ore in the ore-house \ 10 OOLD-BKARINQ MISPICKEL VKINS OF MARMORA. 80 as to demonstrate the effect of rough hand-sorting ; the low assays were therefore of secon il'> 42 14 76 43 7 03 69 10 72 70 10 90 i»0 97 98 !KI KKI 1 101 102 103 104 1 ior> 100 107 1 108 : 109 1 ... 6 33 ... 9 49 ... 17 58 ... 17 58 ... 9 14 ... 5 45 ... 12 83 ... 13 36 ... 4 92 ... 15 11 ... 5 62 ... 28 12 ... 11 95 ... 7 03 17 11 2.5 18 16 17 1 1 44 10 W i 4.5 7 73 71 6 33 72 5 27 19 n 06 20 7 38 21 11 2.-. 22 9 49 46 4 92 47 9 14 48 53 43 73 8 44 74 9 84 75 5 62 49 .■) 62 ' 70 7 :18 77 12 48 78 11 07 79 5 98 23 7 03 24 9 14 25 8 79 50 5 62 51 5 62 .52 17 .58 26 11 2.5 27 8 44 28 18 28 53 13 71 ' 80 7 03 • 81 10 90 82 8 26 54 18 98 .55 8 44 Avt'raKC 10«stiini>k Ohi'ck a.ssays, by 1' Avi-rage valiK' (Jul Average samples, i Average xamples, i s,515 tonsCiatliUffoi rof. Kiehanls, iif Bo iiig i)re, Kast vein, ; ggregaliiig 63 toii.s '1 iggregating 12 tons. e, as.Mayed by .V. Tliie «ilon, ami (tiffiinl, of H.iKi (ler ton. 'utile shaft, East veil Middle vein, *:tt).82. S»13.37gold New York, I, «2-1.88. per ton. «14.73. Allowing the proper proportion of ore-reserve to each of these shafts, the average assay value of the ore in reserves I find to be ;$18.65 in gold per ton. From these most exhaustive tests, the average gold contents of the ore were determined with great accuracy. Perhaps the most interesting and certainly one of the most im- portant and valuable facts developed was the very remarkable unifor- mity of the gold yield of the ore. GOI.D-BEARING MI8PICKEL VEINS OF MARMORA. 11 'I In only three instances — even of second-class ore after the richer ore had been roughly picked out — was less than five dollars per ton in gold found, and the hifj^licst assay of a five-ton lot was S53.4;} per ton. Samples of a few hundred pounds have been fouu^ u> -1>L-^'-. 12 GOLD-BEARING MI8PICKEL VEINS OF MAKMORA. furnaces than in the revolving cylinder, where indeed one cord a day would roast ten tons of ore. There was no comparison, either, in the costof labor in these different systems (in the revolving cylinder it was about 50 cents per ton), and our results give a very decided advantage t<) the automatic con- tinuous cylinder in the uniformity of the roast. It was found that ore which took one hour and three-quarters to pass througii the cyl- inder was thoroughly roasted, so far, at least, as was necessary for amalgamation. The chief objection to the cylinder Wits in the amount of flue- dust made, and that in a somewhat less degree is also the objection to any hand-rabbled furnace. The arsenic fumes are very dense, and when aided by a rapid current of air, they easily carry over dust and gold. The question is not at all one of roasting the ore, for arsenical sul- phurets roast much more easily, more quickly, and sinter less than simple sulphurets; but the important question — the only practical difficulty found in the treatment of these ores — is that of preventing a loss of extremely fine gohl, which is tnechanically carried over with flue-dust and arsenic fumes. This cause of loss, though it will probably always exist to a greater or less extent, does not appear by any means insuperable; but our tests have thoroughly convinced us that, both on the score of expense and loss in flue-dusl, no hand- rabbled furnace is admissible. The automatic continuous revolving furnace, known in the Western States as the White re- volving hearth, an ore which assayed less than .^14 per ton i/icfdrtf, net in ihe huUUm, 91 per ccnf. of the fin'-nnKai/ ; so that it is thought that by care in roasting, from {).'} to 95 per cent, of the gold in the concentrates can be regularly obtained. That the loss in concen- trating will be very small, can be understood when it is considered that the concentration will not be \uin\v close. It is pro|)oscd to crush the ore in rock-breakers to from \ to 1 inch si/e, screen in re- volving screens which will size into say \ to J inch and l to 1 inch, which would then be jigged, the richer ore g<»ing to rolls, and thenci? directly, to the roasting furnace without concentration, and the poorer going to other rolls, where it is crushed, ami then Jigge*!. It is thought that from \ to '^ of the sul|)hurets, and consequently of the gold, will be obtained in the coarse jigging, and will suffer no loss ih concentration. The ])ractical working of these ores I hope to give in another pa|)er at some future time, when the works now building shall have given results on a large scale. The works for the Canada Consoli- dated (lold JNIining Company arc intener ton roasted concent rale.s. $3.50 per ton. Labor is ptiid $\ to $1.25 per day ; wood, $1.26 per cord ; V 14 GOLD-BEARINO MISPICKEL VEINS OF MARMORA. water-power will partly drive machinery. Supplies of all kinds extremely abundant and cheap. The ore carries as an average between $18 and $19 per ton in gold, and assuming a net yiehl in bullion of only 80 per cent., the net profit on the treatment of these ores is estimated at from $10 to $12 per ton. l^^j>\b>ii^'-^ 5^; tefic; It ll ll 3 a- Ik 0' 1 A. Shaft E. Vei u£ T VTs^ lit 400' Tuttlc Shaft E. Vein \ \ Ore» ^ v\ f>. Proi.os«.l Level ProposecTl^vlelTv • I No. 1 \ \ ' Propost'il Level No. -2 Siak 100 ft 1 inch \\ \ \ I'ruiJDHutl Li'vel # i I, MAP OF Catling and Adjacent iMines, HASTINGS Co,, ONTARIO, ^c , , CANADA. ,. ui^^^ .'-.O 100 teoi Mia. En.j. J Transactions of the American Institute of Mining Engineers. I, iiH'f »tV( .. GouJ mill sitT^^lil I'larers ^cv^ tHt MAP OF Catling and Adjacent Mines, .HASTINGS Co,, ONTARIO, ^a, , , . CANADA. „ ,oe*V^" S..J, By U. 11 STIthTCH, feet A>.7.