CIHM Microfiche Series (l\/lonographs) ICIVIH Collection de microfiches (monographles) Canadian Institute for Historical Microreproductions / Institut Canadian de microreproductions historiques Technical and Bibliographic Notes / Notes techniques et bibliographiques The Institute has attempted to obtain the best original copy available for filming. Features of this copy which may be bibliographically unique, which may alter any of the images in the reproduction, or which may significantly change the usual method of filming are checked below. Coloured covers / Couverture de couleur □ Covers damaged / Couverture endommag^e □ Covers restored and/or laminated / Couverture restaur^ et/ou pellicul^e [ I Cover title missing / Le litre de couverture manque I yJl Coloured maps / Cartes g6ographiques en couleur D Coloured ink (i.e. other than blue or black) / Encre de couleur (i.e. autre que bleue ou noire) I j Coloured piates and/or illustrations / D D D D Planches et/ou illustrations en couleur Bound with other material / Reli^ avec d'autres documents Only edition available / Seule Edition disponible Tight binding may cause shadows or distortion along interior margin / La reliure serree peut causer de I'ombre ou de la distorsion le long de la marge int^rieure. Blank leaves added during restorations may appear within the text. Whenever possible, these have been omitted from filming / II se peut que certaines pages blanches ajout^es lors d'une restauration apparaissent dans le texte, mais, lorsque cela §tait possible, ces pages n'ont pas 6\6 film^es. L'Institut a microfilm^ le meilleur exemplaire qu'il lui a 6\6 possible de se procurer. Les details de cet exem- plaire qui sont peut-§tre uniques du point de vue bibli- ographique, qui peuvent modifier une image reproduite, ou qui peuvent exiger une modification dans la m^tho- de normale de filmage sont indiqu^s ci-dessous. I I Coloured pages / Pages de couleur I Pages damaged / Pages endommag6es D Pages restored and/or laminated / Pages restaur^s et/ou pellicul^es Pages discoloured, stained or foxed / Pages ddcolor^es, tachet^es ou piqu^es I I Pages detached / Pages d6tachees \y\ Showthrough / Transparence I I Quality of print varies / D D D Quality indgale de I'impression Includes supplementary material / Comprend du materiel suppl^mentaire Pages wholly or partially obscured by errata slips, tissues, etc., have been refilmed to ensure the best possible image / Les pages totalement ou partiellement obscurcies par un feuillet d'errata, une pelure, etc., ont ^t^ film^es d nouveau de fa^on k obtenir la meilleure image possible. Opposing pages with varying colouration or discolourations are filmed twice to ensure the best possible image / Les pages s'opposant ayant des colorations variables ou des decolorations sont film^es deux fois afin d'obtenir la meilleure image possible. Additional comments / Commentaires suppl6mentaires: Various pagings. This Kern is f ilm«d at the raduction ratio cliaclced below / Ce document est film* au taux de rMuction indiqui ci-dessous. lOx 14x 18x 12x 16x 20x 22x 26x 30x J a4x 28x 32x Tha copy filmed h«r« has baan raproducad thanks to tha ganarosity of: National Library of Canada L'auamplaira film* fut i'i*produit grica A la ginAroait* da: Bibliotheque nationals du Canada Tha imagas appaaring hara ara tha bast quality pcsaibia conaidaring tha condition and lagibility of tha original copy and in Itaaping with tha filming contract spacificationa. Laa imagas suivantas ont txi raproduitai avac la plus grand soin. compta tanu da la condition at da la nattat* da I'axamplaira film*, at an conformit* avac las conditiona du contrat da filmaga. Original copias in printad papar covars ara filmad beginning with tha front covar and anding on tha laat paga with a printad or illuatratad impraa- sion, or tha back covar whan appropriata. All othar original copiaa ara filmad beginning on the first paga with a printad or iilustratad impraa- sion, and anding on tha last paga with a printad or illuatratad impression . Lac axemplairaa originaux dont la couvarture an papier eat imprimia sont filmis an commencant par la premier plat at an tarminant soit par la derni*re paga qui comporta une emprainte d'impression ou d'illustration, soit par la si.cond plat, salon la caa. Tous las autrea axemplairas originaux sont film*s an commencant par la premiere page qui comporte une empreinte d'impression ou d'illustration at en terminant par la derni*re page qui comporte une telle empreinte. The last recorded frame on eech microfiche shall contain the symbol ^^ (meaning "CON- TINUED"), or the symbol V (meaning "END"), whichever appliaa. Un daa symboles suivants apparaftra sur la darniAre image da chaque microfiche, selon le cas: le symbole — ^ signifie "A SUIVRE", le symbols V signifie "FIN". Maps, plates, charts, etc., may be filmed at different reduction retios. Those too large to be entirely included in one expoaure are filmed beginning in the upper left hand corner, left to right and top to bonom. as many frames as required. The following diagrams illustrate the method: Lea cartaa. planches, tableaux, etc., peuvent *tre film*s * des taux de reduction diffArents. Lorsque le document est trop grand pour *tra reproduit en un seul clich*, il est film* * partir de I'angle sup*rieur gauche, de gauche * droite, et de haut en bas. an prenant le nombre d'imagea n*ceasjire. Lea diagrammas suivants iiluatrant la m*thoda. 1 2 3 1 2 3 4 5 6 wr:OCOfY MSOIUTION TKT CHART lANSI and ISO TEST CHART No 2| A -APPL IED IIVHGE '6^J Eost Moin stttei Rochester. Ne, ro-k U6C9 uSA ("6) «82 - 0130 - Pl,„„e "^ (716) 28a - 59e" - t„. ^ "\ ./ A_^ /y-, CANADA DEPARTMENT OF MINES Hon. Louis Coderre, Minister; A. P. Low, LL.D., Deputy Minister; minrn rhancii Eugene Haanel, Ph.D., Director. Magnetite Occurrences Along the Central Ontario Railway BY E. LINDEMAN OTTAWA GOVERNMENT PRINTING BUR-^AU 1913 No. 184 DC Ki k^^^-'\z0 '3 3 e < ANAOA DEPARTMENT OK MINES Hon. Lou^ CoDilliK, MiNisTKg; A I'. I.uw, 1,1,1)., DiriTY MlsnTii; MINRN RHAMrH l.iir.KNt IUam. !*»,l),, DimxToK Magnetite Occurrences Along the Central Ontario Railway BY E. LINDEMAN OTTAWA G O V K J! \ M E N T i' It I N T I .\ G BUREAU 1013 No. 184 LKTTKR OF i i NSMITTAL To Dr. Eugene Haanel, Director of Mines Branrh, Department of Mines, Ottawa. S'.p.- I beg to submit herewith the following report on the maKnetite , lot 57, Hastings road, Tudor township 23 Lot 17, con. XI, Lake township 23 Lots 9 and 10, con. XV, Wollaston township 23 ILLUSTRATIONS. Photographs. Plate I. Pit No. 1, at Blairton mine Frontispiece II. Open-cut at Blairton mines 10 III. Shaft No. 3, Coehillmine 14 IV. Jenkins mine 1* V. No. 3 mine at Bessemer 16 VI. No. 4 mine at Bessemer 16 VII. Open-cut of No. 4 mine at Bessemer 16 VIII. Childs property 20 IX. Workings on iron property at Bow lake 22 VII. Maps. Page 185 — MaRnetomctric map of the Blairton mine End. 185a — Ck'ologiral map of the Blairton mine * ISfi — Magnelomelric map of the Belmont mine " IStia — Geolojjica! map of the Belmont mine " 187 — Magnetometric map of the St. Charle-; mine " 187a —Geo!' i:;ical map of the St. Charles mine " 188 — Magnetometric map of the Baker mine " 188a — Geological map of the Baker mine " 189 — MagiK'tomeii'ic map of the Ridge property " 190 — Magnetometric map of the Coehill and Jenkins properties.. . " 190a — Geological map oi the Coehill and Jenkins properties " 191 — -Magneiometric map of the Bessemer properties " 191a— (jef)logical map of the Bessemer properties * 192 — Magnetometric map (jf the Rankin, Childs, and Stevens properties " 192a — Geological map of the Rankin, Childs, and Stevens proix;rties. " 193 —Magneiometric map of the Kennedy property " 193a — Geok)gical map of the Kennedy property " 194 — Magnetometric map of the Bow Lake property " 204 — Index map showing magnetite occurrences along the Central Ontario railway " MAGNETITE OCCURRENCES ALONG THE CENTRAL ONTARIO RAILWAY BY E. Lindeman Introductory. An investigation of the magnetite deposits along the Central Ontario railway was commenced by the Mines Branch in V.HKt, when a magneto- metric survey of the Belmont iron mine was made by B. F. Haanel.' Dur- ing the summer of 1908, H. Frechette made a niagnetometric survey of several ore deposits near Bessemer and Hermon,' and in 1909 Mr. Haanel again visited the district and examined some of the deposits along the rail- way.' During the last part of the field season of 1910 a magnetometric survey was made by the writer, assisted by W. M. Morrison, of No. 4 deposit at Bessemer. In addition to this a topographical and geological map, including all the ore deposits at Bessemer, was made. During the summer of 1911 the field work was continued and visits were made to as many as possible of the reported deposits of magnetite along the railway. The ix)ints visited were as follows: — I I I I II V Blairton mine Lots 7 and 8 Con. Belmont mine Lot 19 Maloney mine Lot 18 Lots 12, 13, and 14. " Lot 17 'I Seymour mine Lot 11 St. Charles mine Lot 19 " XI Tudor Horton mine Lot 57 Hastings Rd. " Lot 17 Con. XI Lake Lots 19 and 20 " IV " Baker mine Lot 18 " XVIII Tudor Emily mine Lot 7 Lot 8 Coehill mine Lots 15, 10 Jenkins mine Lot 17, 18 Lots 9 and 10 Ridge Lots 17, 18 Lots 16, 17 Lot 28 Bessemer Lots 1-5 Rankin property Lot 10 Childs " Lots 11, 12. Stevens " Lots 13, 14 Kennedy " Lot 17 Lot 30 Belmont township. 11 11 Marmora " 11 11 11 11 Madoc " Bow lake XIX " XV " VIII Wollaston VIII XV H III XXVIII Chandos VI Mayo IX " IX " IX " V and VI Carlow XIII Dungannon . Lot 21 "X and XI Faraday See Sum nary Report of the Superintendent of Mines for 1906- Mines Branch for litOs. ■■ 1909. The Kt''»l"Ki'"'il features of the \ari()us ore deposits wore stii(lii), St. * .arles mine, Baker mine, RiJue proiK'rty, Coe! ill mine, Jenkins property, Rankin " (topoRraphy), Childs " ( " ). Stevens Kennedy " Bow l-ake " In this work the writer was assisted by Messrs. W. M. Morrison and O. G. Gallagher. As most of the ore deposits visited arc altogether or partly covered by drift, the magnetomctric survey has been of great help in ascertaining the probable area within which the ore is likely to occur. The general plan of the survey was as follows: a base line was first laid out, approximately following tl;e strike of the or(^ deposit, and carefully chained. .-\t right angles to this line, at iiUer\ als of e\er\' ,50 feci, cross lines were run to the limit of the disturtjed field. These lines were staked every .')() feet. In this manner the whole area to be investigated was laid out in snuares. The magnetic observations were taken with a Thalen-Tiherg magnetometer. The distance between the points of observation varied from 2.5 to 100 feet, depending upon the local complication of the magnetic field. Fhe readings in degrees as observed in the field were reduced to values corresponding to an angle for a magnetometer with a constant of l.H'. The reduction of the verti'jal angle was done according to the following formula :— tgV=k„tgV.. V = the angle which corresponds to the angle V„ for an instrument with constant l.H. V„ =1 angle observed with a magnetometer with a constant k„H. The isodynamic lines of the accompanying rr.ignetic maps have been drawn in a similar wa\- to that in which contours of < ' vations are made. In order not to overload the map witli too many lines, which would obscure rather than emphasize the salient filatures of the deposit, the 10 and 30 degree curves have tieen omitted. The colours used in these maus are, blue for positive or north pole attraction, and yellow for negative or south pole attraction, and the areas liciween the bounding curves are laid in with appropriate tints. The topographical survey was done by means of plane table and stadia, or b\- transit and stadia v.hen the country was thickly wooded . ' I!=ljoiizuiit.il ctjinpon'-nt of the ■ .ifth'- i! . jiiieiic fi,;l(I. CHAPTER I. LOCATION AND HISTORY OF THE DISTRICT. The iron ore ocrurrcnces covcrtnl by the present report are situated along the Central Ontario railway, between Central Ontario Junction and the village of Bancroft, a distance of W) miles. The distance of the various deposits from the railway varies from 12 miles down to a few hundred feet. Some of the iron ore deposits in Hastings and Peterborough counties have been known for many years, and as early as 1K20 an attempt was tn.ide, at Marmora, to manufacture pig iron from magnetite taken from IMairion mine. The venture does not seem to have met with any success, however, and operations were discontinued. In 1807 the Rlairton mine was opened up again and mining was carried on from time to time until 1S75. In 1882 tiie building of the Ceiilral Ontario railway was commenced, with the object of opening up the nuiner- ous iron ore deposits of .North Hastings. At this time mining operations started at (\)ehill and in several other places, but it was soon found that the magnetite contained so mucli sulphur as to be unmarketable, and the mines were closed. In 190t) a part of the Bessemer and Barrys Bay rail- way was built, connecting the ore deposits at Bessemer with the Central Ontario railway at a point about one mile south of L'Amabh- station. Mining operations were carried on by the Mineral Range Iron ('(jinpaiiy, until the beginning of 1908, when the properties were leasetl to the C anada Iron F"urnace Company. This Company continuefl operations until April, 1910. In the spring of 1911 the Bessemer, Childs, Coeiiill, and Blairlon properties were ac- quired by a corporation known as the Canada Iron Mines, Limited. This new Company commenced mining operations at Bessemer in August, 1911, and intend to erect in the near future a magnetic concentration plant at Trenton for the treatment of their ores. The total amount of ore shipped from Bessemer up to the end of 1910 was 83,55;j tons. with CHAPTER n. GEOLOGY OF THE DISTRICT. Thf greater portion of the area is <.( riit)ifil l)\ Arciui-an rocks, ronsi^t ins of crystalline limestones, iiiterstratilu'd with a siriirs of paraRneisses anc schists, and intrudwi l>v various i^meous rocks such as granites, syenites diorites, amUahbros. thitlie denuded surface of these .Xrcha-an nn-ks th( various si-tliinents constituting tlie lowest beds of the Fahcozoic series hav( been dcpositwl. The latter are found in the most southerly poition of ih« area, forming a more or less continuous sheet, coverin>j the older rocks The crystalline limestone of the district Kcnerally has a coarse texture ami i more or le.-- impure, owing to \\w prest-nce of various -ilicates. Some of tli( paraKneisses are likely to represent alterations of more or less highly argij laceou- s<-diments. while others are rich in quartz and sc>em to make transi tions to true quartzites. Associate*! with the paragncisses and often passing into them are darl coloureil basic schists, which have been grou|)ed by Adams and Barlow unde the general name of ampiiibolitc.' Their chief constituents are horn blende and feldspar, but pyroxene and biotite often take the place of th hornblende in part. The granites of the area generally have a coarse texture and are gre to reddish in colour. They show for the most part a distinct foliatioi though in many places the foliated structure gives way to a granitoid on« and every stag*? of transition, from a typical granite to granite gneiss, ca be seen. The syenites have a coarse texture and are of a reddish coloiir, thei chief constituent being a red feldspar. They often seem to grade into tli granite and granitic gneiss and there is good reason to believe that the>' ai simply a differentiation phase of the granite magma. The gabbros or diorites have all the character of great basic intrusior and are generally perfectly massive. Like the granite and syenite, they ci through the limestone and associated gneisses and schists, sending dykeiil masses through them holding inclusions of the same. 'Sec Memoir No. l> uf the Gtologicil Survey, Canada. CHAPTER 111. ORE DEPOSITS. The magnetites of the district may be divided into two groups: - (1.) Magnetite occurring along or near the contacts of limestones and schists with various igneous riKks. (2.) Titaniferous magnetite associatefl with gabbro eruptives. Contact Maftnetlte Deposits. This type of ore (Kcurs as steeply dipping lenses and irregular masses interbanded with cr> stalline limest:me and various schists aUmg or adjacent to the contact of the latter with some igneous rock, generally diori e. Asso- ciated with the nagnetite are numerous ferrugit.ous silicates such as pyro- xene hornblende, epidote, anhill, pyrrhotite. In some cases the pvritous portions can be separated bv cobbing the ore. while in others the sulphides are so abundant and so finely ui.tributed throughout the ore as to render its elimination by such a proress "nP'^^'l^'f • The phosphorus in the samples taken varies, with one exception, from Ul» to 0200 per cent. It is very difficult to estimate with even an approximate correctness the quantity of ore axailable in this district, because of the lack of sulhcient development and of the exceedingly irregular charater of the ore b.xlies. It seems, however, as if, so far, this feature had hardly bc-cn rccognueO sufficiently, as many property owners assume that the ore occurs m regular 6 Th<- follnwiiig tal)lL> hIiows tlu- unalyscit o( itoiiu- of the mugiict itcH bvlong- ing tu ttiis cluss: a 2 S S S « 8 * J.1|)V111 omn|(j«ui '(HS euiiuniv 0»D •0!1 0»J °aOJ| 3IIIB13[^ T3 c o S S 8 .^ S S H 2 3 S •■*_ 3 S e o e b e o 3 fi '* 3 : « » «2 S g S a fi ■N « « ^ s f t- 8 : ^4 M »H M 8 8 s s o ^4 30 !-• o e e e 3 — c^ r^ w5 jN w « a? S ?i uj S '2 g '2. U" ? s S s ^ 3 ?i o o o o — fl "- © — e e b o b b r e = s S 8 « ?• o beoocobbbsbb'^ S.^ M 00 t- 15 t M M CI O CO -S e o u X - X X r L X X X •: o u c c o u c o X, o vH v^ rH F<4 ^^ ^ 2 = 2'^?; 1 I ■^ 2 s 2 03 = E "i E 5 £ s - •= E ^ E 5 CQ CO u A y- e o a 2 a 2 s' c 2 a o e 3 U. e 2 4 6 ■2 '.a a a 3 •= o .§•8 "I ^^ = "3 ■~ s >, a 1 S & 1) 2 2 > > < < 7 Ik-*!', aiul ihurcfronnTroiu-ousls infer tin- <<.iuiniiii\ <.l tluMli'|).»it*t lH,'twei>n wiflf ly Hi-paraiitl outcrops; in somi- rUM-, most f\aKv; Ii.im- 1 fon (requvnt in u>iiiK the clip ntHtlle. If. for in-taiite, a f.w Im^Ii niaKm tie readiiiL;^ liav.- Invn ol)tawifniltt the ore to a mannetic coiuentration pnxess. It may l>e that no sir deposit contains ore reserves lar^e enouKh to warrant the erection ol a c centratinR plant of sutficlcnt capacity to ensure the profitable worklnf such a process, but should further development confirm the extu'Ctat which the result >f the investigation of sttme of the aljove-mentioned deix) indicate.-, by a i onsolidatlon of soin', .A these properties, It shoulhur >rc' tk'fK)sit9 linn nanRue 1 mc)>sits in the Mubinitting tt no single on ol a con- working of fxjK'ctation ntildi-posits 1 Ih- [Kjssible ike till- erec- above mcn- A large per- fine in order ited gangue- e ore can be g process. CII\PTER V. DESCRIPTION OF MAGNETITB OCCURRENCES. Blairton Mine. The Blairton iron mine is situated on lot 8, conresstion I. township of Belmont. PeterlM)rough rounty. at the southwest ewl of (row lake, aliout 5 miies west of the village of iNlarniora and about '.\ miles northeast of Blair- ton station on the main line of the Canadian I'arifu- railway. The first mining operation-, at Blairton date back to 1820, when ore was mineth r American points. According to the books of the Company, 12,747 gross tons were sliipped 1.1 1808, and 15.440 tons in 1869. From November, 1872, to the end of Scp- temlK'r of the following year, 4,.58G tons of ore are reportetl by Mr. J. E. Aunger of Blairton to have been shippcfl. The mine was worked contm- uously from 18fi8 to 1875, but no information regarding the total amount of ore mined d' ring this period is available. The cost of mining is reported to have been .ibout SI. 25 per ton. and the transportation charges from the mine to Pittsl rgh $4. Notwithstanding the excessive cost of transporta- tion, mining rations could be carritni on with some profit on account of the liigl price of iron ore. A change in the iron ore market, however, soon took place and lower prices prevailed. This fact , coupled with an increased duty on l.on ore going into the United States, prevented o()erations from being carried on profitably, and the mine was closed in 1875. Since then, no attempt has been made to recommence work, and at the present time all the old workings are filled with water. The area embraced in the accompanying map (185A) is chiefly occupied by Archaean rocks made up of dark-coloured hornblende and chlorite schists and crystalline limestone in contact with diorite. The general strike of the stratified rocks is about N. 15° VV. with a steep dip towards the cast. In several places beds of limestone underlain by conglomerate and constitut- ing the lowest strata of the PaUeowic series are found overlying the .^rchxan rocks. In the conglomerate small pieces of hematite are often found em- bedded. The main deposits consist of magnetite. They occur in the older Archaan rocks along the contact of the crystalline limestone with the diorite. The hornblende and chlorite schists are found in the northwest part of the area outcropping in several olaces aloni{ the shore and on the north and northwest sides of the big hill near the lake. 1 hey often show a porphyr itic 10 texture, with plu'iiocrysts of feldspar in a dark fine Krained pround n East f)f tliese sciiisis and ninfornialile to tlieir iK-Miii^ plane lies a he (Tyslalliiie lime>tc)ne. Farther east tiie greater [)arl of the area is occii !)>■ diorite. Tiic latter generally has a coarse striirliire, but becomes so fine ura rear its contact witti the crystalline limestone as to make it impossihl distinguish with the nakerl eye the chief mineralogical constituents of rock. Kpidote is, however, often present, and iron pyrites is also of (juent occurrence. The magnetite occurs associated with this light g inetamorphic rock. In some parts of the field it is foimd in well del layers interstratified with the rock; in others finely disseminated tlirougl the same. The (juality of the ore may best be judged from the following ana representing an average sample of the ore taken across the ore bod; the north side of pit No. 3: — Iron 50 10 per cent. siiica.sio..' 9-88 ;; Phosphorus 004G Sulphur 1'42 " Titanium, TiO, 10 Lime 3 '52 ^^ Magnesia 1 '('4 __ Alumina l'7'i Judging from the magnctometric survey, the ore occurs iii two sep; areas On the more southerly of these areas ore has been mined fron open pits N-. 1 and No. 2. The total area of these two pits is 2 square fei't. The depth of pit No. 1 is 125 feet. By a diamond drill the deposit has been proved to a depth of 550 feet. The other area ha^ been opened up by a large opeii-cut on the hi near ("row lake. Judging from the magne'.ometric survey (see map the total lengtli of this deposit may be roughly estimated at about 560 its northern end extending about l.'?0 feet under the lake. On the hi immediately west of the open-cut several strongl\ positi\;e magnetic f alternating witli some strong negative ones, indicate an irregular dist tion of the magnetite throughout the rock. Tlie total area within which ore is likely to occur in this part o field is roughly estimated at 128,000 ^(luare feet, but no doubt a percentage of thi.: area is occupied ))>' barren rock. The Belmont Iron Mine. The Belmont iron mine is situated on lot 10, cit is of irregular shape and has a 1 *,.? .'-§^^^ [round mass, lies a holt of a is occupied ) fiiK' uraiiied mpossihle to tucnts of tiie i also of fre- s liRht green well defined d throughout iving analysis ore body on two separate ned from two pits is 27,.J00 ond drill hole )n the hillside ^ee map 18o), bout 500 feet, )n the hillside aguetic areas, 'ular distribu- is part of the loubt a large c I, of nelmont, It is coimected s the Ontario, ne to the On- kin^s are siui- a siiaft. The 1 -(see acc-.jitl- id has a length I 11 of about 220 f^-el in a north and south direction, with a widlli ranjiinK from 40 to 70 fet-t. The (kT'tli "f ''>f P't '^ from :i to 20 iec-t. About la feet north of pit Xo. 1 tlie main shaft is beiiiK sunk. The de|nh of the shalt, at the time of tlie writer's visit, was 32 feet and from its bottom a c.riU 3'' feet long was said to have been driven under pit No. 1. 1 it No. -, called the Nickel pit, is situated about 100 feei southeast of pit No. 1. It is about 00 feet long and 40 feet wide, with a depth ranging from o to b feet. The ore consists of maijnetite associated wi^h pyroxene, chlorite, and some calcite. It occurs along the contact of crystalline limestone and dior- ite A few outcrops of crystalline limestone are seen on the south wall ot nits No 1 and No. 2, while the diorite is well exposed on the small knolls west of the railway track. The character of the diorite vanes from a grey, medium grained rock, made up chiefly of hornblende and feldspar, to a dark cuarse grained variety, the chief constituent of which is hornblende carry- ins; sonie magnetite and iron pyrites. The west part of the area embraced bv the map \f occupied by dark coloured, fine grained rocks, generally with a'schistose structure. Similar rocks are also seen in several places on the knolls east of the railway track, where they are found as fragments of vary- ing size embedded in the younger diorite. The character of the iron-beating formation varies consideralily. In some places it consists of almost pure magnetite, in others of a rnixture ot magnetite and gangue minerals, chiefly pyroxene and chlorite; in other places again the latter minerals prevail almost to the exclusion of the magnetite. Iron pyrites is frequently seen throughout the ore. The following analysis represents an average sample taken by the writer across pit No. 1 at the north end :— Iron 5120 percent. Silica 1210 ;; *" losphorus 0032 ^^ Sulphur 034 Titanium, TiOj 10 Lime, CaO -iS? Magnesia, MgO 3 93 Judging from the magnetometric survey (see map 186), confirmed by a few natural exposures, the area within which the ore is likely to occur may be roughly estimated at 43,000 stiuare feet, but a large percentage ot this area is undoubtedly occu'.ied by barren rock. The Maloney Mine. On lot IS, CMiicessiMn I, of Marmora, a few hundred feet south of the Ontario, Belmont, and Northern railway, a deposit of magnetite has been exposed. The workings consist of two open pits and a stripping, t^^'tween the three workings a magnetic attraction exists for a di,tance of about JW feet. The uio !>odv, as cxp.):^ed ill the main pit, ?!vr,vs a width ot .-ibout 15 feet. It consists of magnetite mixed with a considerable amount ol gangue ^%1k^'^- 00 per cent. 03 It 137 ti 500 u 250 II 12 minerals. An average sample of the ore taken by the writer gave tl lowing analysis: — Iron 47 Insoluble 21 Phosphorus Sulphur Titanium, TiO, On the hill immediately south of the workings, numerous outer gabbro-diorite can be seen, while an outcrop of crystalline limeston observed near the railway track to the north. Lots 12, 13, 14, Con. I, of Marmora. The greater part of lots 12, 13, and 14, con. I, of Marmora, isoci by a coarse grained gabbro-diorite, cut in the most intricate mam a red granite and pegmatites. Along the contact with the latter rock netite in small quanti>="«! is found in several places disseminated throu gabbro-diorite. Whc , he magnetite has been found, the magnetic i tion is, however, very feeble and the discoveries so far made are economic impwrtance. Lot 17, Con. II, of Marmora. On a hill running east and west, on lot 17, con. II, of Marmot test pits have been sunk about 150 feet apart, showing some magneti seminated throughout a gabbro-diorite similar in character to tha on the Maloney property. The distance from the workings to the O Belmont, and Northern railway is about 500 *^eet. An average sample of the iron-bearing rock gave the fol analysis: — Iron. 34 Insoluble 43 Phosphorus Sulphur Titanium, TiO, 80 p- cent •80 II 134 II 410 II 10 II Seymour Mine. The Seymour mine was one of the earliest producers of iron on district, but has been abandoned for many years. It is locatecl on i half of lot 11, con. V, of Madoc, about 4 miles north of the village name. The old shaft is said to be 125 feet deep. The old open-cut has a length of about 200 feet with a width i from IS to 2r> feet. The ore consists of a fine gr.iined masrnetite. ass with chlorite, pyroxene, and hornblende. It " -rounded by a laru,e eruptive. The magnetic attraction near * kings is very v/eal r gave the (ol- us outcrops of limestone was 3ra, is occupied ite manner by ttcr rocks mag- ;cd through the agnatic attrac- -.ade are of no Marmora, two magnetite dis- r to that seen to the Ontario, the following It. [ iron ore in the ited on the west e village of that 1 width ranging elite, associated y a larsie granite ery weak. 13 St. Charles Mine. The St Charles mine is situated on lot 10. con. XI. of Tudor, abou^ l,.lf ^ mile' west of McDonald sidins on the Ciutrat Ontario radway. ThcNv<.rknusa;nsist.,ll.ve..,u'n pits (see acrompany.nK maps, 1S< anu 87aV The ore is niap,etite, ass..ciated with mure or less ^an^uc' .nmorals. uch as parnet. hortd.l. nde, ps roxenv. and caUi.e. It .K-,-urs alon, the con- tact o rrvstalline linuslone with a medium to hnc uramed dion o. Hiere Ire aca.«linR to tlu- plan .,f the maRnet.Mnetru- survev t hr.e deposits on d,e orone tv On the principal .k-p ,sit pit. N.^s. and 2 have been made. Srong magnetic disturhanc.; exist along the hillstd. tor a .l.stance of .520 Set The total area within which magnetite is hkely to occttr is roughly est mated at i:J,500 square feet. A considerable portu.n of this area, how- cir contains ore which is either too low in iron or has too much sulphur to be suitable for iron smelting without previous concentration. An average sample taken by the writer across the ore body at open- cut No. 2 gave the following analysis:— Insoluble 3185 per cent. Iron 4200 Phosphorus 080 Sulphur 832 During the season of 1900, 3,000 tons of ore are reported to have been shipped from this property to the Hamilto. -n-^e The iron content of this ore varied from 57 to 60 per cent, wh; ..phur ranged from 5 to 1 per cent. Baker Mine. The Baker mine is sitiiated on lot 18, con. XVIII, of Tudor, about If miles west of Ciilmour station. The workings consist of three open-cuts and a numb-r of test pits on the eastern slope of a ridge running north and south. The ore is a hue " a ned magnetite, intermixed with a large amount of gangue ma ter. iX pyroxene and chlorite. It occurs along the contact of crystalline imesi'oiH and diorite. Iron pyrites is of common occurrence in the ite s well as throughout the ore. Judging r..m the accompanying a'"et .metric map (see map 188), the ore occurs in small detaciied bodies o t<^kets. The largest area of strong magnetic attraction is tound arr.und open-cut V... 1. The elevelopir.ent work done here has, however, so far failed to reveal anv ore of economic importance 1 he ore body op-med up by open-cut No. 2'has a width of about 2.^ leet, hut the magre ometnc ur- vev imli,a,es that it. .•xtent is very small. W<„-k,ng No. .5 shows any! e^ small pocket <.l magne.ite along the contact of crystalUne lune.ume aitd diorite. An average sample taken across the ore body at opejt-cut No. 2 gave the following analysis: — insoluble :57 10 percent. Iron •^^■'Z' Piiosphorus iU ^^ Sulphur '^ '-^^ 11 Lot 28, Con. I, of Chandos. On lOt 28, con. I, of Chantli's, an opon-cut, .W by 21 fi-i t, ha- made into a liill, i-vpusiiiK a dark coloun-d amphiholito, a>-;niiatiKl some rna^jni'titf. MaRiKtir indications of several other depusils i iniincdiaic vicinity were also noticed, hut they all ai)peareti to be o sn': 11 extent. The Emily Mine. The Emily mine is sitiiatwl fni lot 7, con. XIX, of Tiidor. ab< miles northeast of dilmour station. Chapman, in the 'I'ransactii the Royal Society of Canada, 188."), section III, p. 12, describes thi magnetic ore deposit of considerable e.xtent. He says: "T!ie e; ore rises in a series of ledges from the level of tlie ground to a height « 150 to ISO feet, and extends over a sjxice of at least 1,000 feel in by 100 feet in breadth." This could not be verified by the writei lot 7 a somewhat abrupt ridge, chiefly made up of a coarse grained gi was found. A large open-cut had been made into the hillside, show places some small patclies of magnetite heavily intermixed with j matter. The magnetic attraction around the open-cut is also very irn Lot 8, Con. XV, Tudor. On the east .-^ide of a ridge running approximately north and so lot 8, con. XV, of Tudor township, several strippings have been made ing a grey granite in contact with chlorite and hornblende schist. As ed with the schist are narrow bands of magnetite. The magnetic atti is rather strong in places, but none of the workings has so far reveal ore body of sufficient size to be of economic importance. Coehill Mine. This mine is situated on lots 15 and 16, con. VIII, of Wollasto is connected by a branch line, 7 miles long, with the Central Ontar way at Ormsby Junction. The distance by rail from the mine to 1 is 73 miles. Mining operations at Coehill were begun in 1883 and were car for two years. During this time, 80,000 to 100,000 tons of ore are r( to have been mined. On account of the high sulphur content, rei the ore unsaleable, mining operations were, however, discontinued i; and a large percentage of the ote mined is still lying in stock piles at th In 1885 Mr. Coste reports the depths of the three shafts to be : Ni feet; No. 2, l.SO feet; and No. 3, 100 feet. In 1901 about 10,000 ton are reported to have been shipped from the stock piles. All the ok ings are now filled with water. The main ore body is well exposed hill north of the railway track by two open pits. The general trenc formation is northeast-southwest, with a dip of about 50 degrees t the southeast. The deposit seems to form part of a limestone ampi series, locally enriched in iron by the intrusion of syenite, which c scries in the most intricate m.anner. The ore consists of a fine *^P«yi:- ffi t, lias hi «'ii sSDciatcd witli i-pusils in tlic tbe : No. 1, 95 ),000 tons of ore 11 the old work- exposed on the 'ral trend of the legrecs towards ane amphiboiite which cuts the : a fine grained T. 1ft maBni-titc, aworiatcl uilh homhlcixk-. pyn.x.n... aiul caUii.-. ''»'»;" SS-i . r .tratifu-! aj-iuarana- paralUl tu tl..- -tuU-. .Ins h .Iu.- to , va iat . n in tin- nlaliv. .a.mn.nt of ihi- cmsiiuuni m.n.ralH |,r.s..nt. Some andlmrnhii- .1. . Tlu- av.Ta«o sulphur c.nt.ul ..f t ,.• or... \mU a . onsu - ^ , Tn oun -f iron pyriu-. an.l pyrrhotiie Uinu .l..sfmuuU.- to -0 eet n a.ld - lengui oi a several other Jeposits all covere, the o,h>.. pit on lot 18. PM^^V le The Ridfte Property. The property reforrtcl to iiridfr thin name h Mituated ni-ur Ridgr office, about lH mil«'"« south <»f Corhill, and iii III, ami lots Hi anil 17, roii. Il.of Wollaston lownshin. Tin- ariM is h drift rovcri'd, and th»' only rxposurt' of m.iKnt'iiti' ho far found i-i >iiiua lot 17, ((»n. 11. HiTi' a thill band of m.innctitc, lyiiiK in mica and blende sthjst, has Ui-n rt \iali-i of ilie hill. F up the hill side, a niutainorphir riKk, rliirfly made up of gariut, i« m contact with the name itchist. On lot 18, con. Ill, a test pit is rc|)orte miles. In KHKialiram called the Bessemer and Harrys Hay railway, w.is built, loiuiectii village at Bessemer willi the Central Ontario nilw.iy, al a point al mile south of L'Amable station. Mining oiK'ralious were urried on 1 Mineral RauRC Iron Mining Company until the beginning ot lOOS, wh properties were leased to tJie Caiiad.i Iro.i I'urn.ui' Conipaiu. Company continued operations until Ai)ril, 1010. wluii llic lease was' al to expire. In the spring of 1011, the Bessemer pro|>erties wcr*' ac( by the Canada iron Mines, Limited. Tlii^ Com(>aii\ odumeiHeii i operations at Bvssemer in August, 1911. and is now erecting a ma concentration i ant at Trenton, for the treatment of the ore. .-* v? CiiT'^^m'?'^ "i iir Ritlge punk tliruuKh f is a consider- east and west i( hpe. Its (luality varies greatly in different parts of the deposits. In come Cu--,es a clean magnetite of iiigh iron content is observetl; in others, the niagnclito is closely associated with garnet, hornblende, epidotc, and calcite. and the ore often appears to oass gradually into such ganguc minerals. The best ((ualily of the ore averages alioui 5t [ler cent of iron, but considerable ctjbbing has to be done in ordir to keep it up to that standard, as a large perceniage of the ore does not average more than 40 to 48 per cent of iron. This latter ore has so l.ir been relegated to the waste dumps, or left in the mine. Locally, stringers and patches of iron pyrites are found, but by hand cobbing the ore it lias been posssible to keep tl.e sulphur down to somewhere near 007 per cent. The jjercentageof phosphorus is very low, averaging from UOIO lo 0025 per cent. .'Vn average analysis of the shipping ore, given by the Canada Iron Fur- nacf Company, Midland, Ontaiio, is as foi. ;: — Metallic iron (Fe) 54 29 per cent. Lime (CaO) GSG Magnesia.. . (MgO) r35 " Alumina {.MOO 202 Silica (SiO.) 984 Phosphorus .(P) 0-010 Sulphur (S) 0062 IS An av.raL'r a^aK^i^ <>i '.'' larluads sbii^ind t.. Mulhuul diirin I'.HH is as fnllow-;: • Iron ■"'^■*' [wrcont. Siilpliiir I' •'"■■' I'lios!)li()iiu 022 Two avcravH- ■samples of clisranl;.' " i:vo,) Maanesia 4 07 ;; 2 .SO _^ Alumina 2:M - . Silica l.V;U) " 1 20 Fliosphorus 004 '• 0.0 Sulphur 03 " 30 The ore Ixxlies occur in four groups, wliich have been .lesignated on the map as No. 1, No. 2, No. 3, and No. 4. (See maps 101, 191 A.) The magnetometric survey made on the south half of lot 1, con. \ II, indicates the presence of a number of small ore lenses. On one of these a pit has been sunk, and a small .iiiantity of ore removed. The ore is badly mixed with gangue minerals, cliiell> hornblende. The other deposits indicated by the magnetic map on this lot are all drift covered. On lot No. 2, con. VI, an open-cut, known as No. 2, has been made a short distance north of the railway, revealing some magnetite interniixed with various gangue minerals. The magnetometnc survey indicates, how- ever, ihis deposit to be a mere pocket. It also indicates the presence of a few other small deposits east of No. 2. No. 3 mine is situated on lot 3, about 1,300 feet east of No. 2. It con- sists of two open pits, which have !)wn opened up on two ore lenses, separ- ated from each other by about .W feet of gangue rock, through which a small amount of magnetite is disseminated. The ore body dips at an angle of 70 degrees to the southeast, the hang- ing wall being amphibolitc. On the hill immediately south of the workings intrusions of granite are seen in the aniphibolite series. In addition to the two ore lenses of No. 3 mine, the magnetometric survey indicates a short distance east and west of these workings, several other deposits, all of which are, however, covered by drift. No. 4 mine, the principal deposit at Bessemer, is situated on lots 4 and 5, con. VI. It lies in the limestone-amphibolite series, near its contact with the granite. According to the .magnetometric survey, the total length of this deposit mav be estimated at about 1,000 feet, its western end ex- leiiaiiiK 400 feet under Lilile MuHet lake. The average width nf the deposit is roughly estimateil to be about 50 feet. all l'» So i.ir. iho niininu c>pcraiii)us haw' lic.-ii (Miitim-il t'> ilir ca-ii-rn lialt of tlu" tli'posii, and till- «n .Iter n.irt of tlie i^k' t.iki'ti I'roni an open-cut 2u'> fell lonK, U) to (10 feot wide, and with a nia\i:mini d.^piii of aboui t'lO I'lyi. At 'lilt; wi-st end of tho oju'ri-cut, an iTu-iincd ;.liafl lias iicrii sunk, follinvini; the dip of till- on- ijody. The vertical denih ol tho shaft is 100 feet, with stations and k\cls cut at a depth of ')<) an(' '.) t feel. ( )re has also been mi. led on the '-.est side of the sliaft, v''ere, for a distance "'i about 100 feet, the ore has been stoped out between i.ie ")() i-nd 04 ft. level-,. In width, the slope varies from 2!) to 17 feet, with its north side still in ore. The ore is lure, however, of low KrMU\ hisjhly iiii.xwl with uaiiKUc minerals, and also carr\ ini; a rather high percentage of iron f yr't^'^- ^"'1 'i^**- llicn.-fore, been left. JudKiiiR from the results of the maKnetonietric surveys, contirnied l)y tlie distribution of a few natural exposures, we may estimate tlio total ore area of the seven lar^;est deposits to be about SIl.tJOO scpiare feet, of wliirli 50,000 are attributed to No. 4 dcpi^sit. This estimate does not, however, pretend to be more than a \-ery rough approximation; besides, a considerable portion of this area contains, no doubt, ore wiiich has too low iron content to bo suitable for economic iron smelting without previous concentration. In order to ascertain the suitability of the ore for magnetic concentra- tion, tests have been made at the ore concentrating laboratory at Oaawa on a shipment of lo tons of discarded ore fr.im No. 4 mine. The sample was crushed down until -JO per cent of the ore passed througii 200 mesh, aiid separated by the CJrondal wet process. The i-sult of the lest is siiowii in the following table: — Analyses of Crude Ore, Concentrate, and Tailings. Crude ore. Tails. Concentrates Iron 30 oO 4 ' u 67 ' 4 Insoluble matter 35 157 . . . 5 87 Phosphorus 02G ... 007 Sulptiur 0-314 ... 0185 Lime -'jfJS ... Magnesia 0030 ... It will be seen from the above figures that 1'96 tons of this material are required to make 1 ton of concentrate with an iron content of 67'4 per cent. The percentage of iron in the crude ore saved in the concentrate is 94 per cent, while about 6 per cent of the iron content of the ore is lost in the tailings. The phosphorus, although below Bessemer limit, in the crude ore, has been depressed to a point that should make the concentrate very valuable for the production of special low phosphorus iron. Rankin, Childs, and Stevens Properties. The workings, known locally by these names, are situated on lots 10, 11, 12 and 13, con. IX, of Mayo, about 25 miles northeast of Bessemer and about 1 mile south of Herman post-office. The area is chiefly underlain b-y a fine grained mic.i -rliisr .ind a lime- stone-amphibolite series intruded by granite and other igneous rocks. ''-y^^rr 20 Tlif on- ilfpo-it^ ornir associalid with llic S(hi^,t and aniphibnlito scri.-s mar the contact of tlio iy-iifou!. rocks. niits of ore arc very starco, the greater part of the area hcin^ licavily drill comtiiI. The i;oiural sink" of the i.on licarinj; formation is northeast -southwest witli a steep ilip to- wards the southeast. The approxiniate location of the various ore deposits is shown on the accompatninj; map, l(t2A. On the Rankin property, lot 10, con. IX, considerable stripping has been done e.xposinj; magnetite associated with hornblende and cldoritu schist over an area of MM feet X tj8 feet. On the Cliilds property, lots 11 and 12, con. IX, 4 openitii^s l,.ive '.x-n made No. 1 is a .surface stripping on the road allowance between .ot il, cons. Vlil and IX. It shows a dark coloured hornblende schist inipreKuatcd in i)laces with ma«iieiiie, ami intruded by an igneous rock carrying epidote and garnet. No". 2 consists of an open-cut on the hillside. The face of the cut is 2(i feet wide and shows magnetite intrrmixe !^7 Phosphorus 104 Sulphur 215 Lime... S 08 Magnesia 1 "4 Tilaniuni 10 Childs. per cent. 42 00 12 5;5 (I ()(j() 1()0 i (.) 2 00 10 Stevens. per cent. :50-70 2:5 00 OSO 015 \}. 2 £ '±iSBUt 21 Concfntraling tests on a shipment of ore, 1 89 gross tons, from ilic Childti property, gave the following result: — Analyws of Crude Ore, Concentrate, and Taillnita* Crude. Iron Ins(>lul)le matter Phosphorus. Sulphur Lime Magnesia Concentrate. .35 3«S 8 083 04.5 5 8:^ 41 66 4 () 09 016 022 Tails. 5 7 The ore was crushed down until fiO per cent of the material passed 100 mesh, and separated by the Grondal wet process. Kennedy Property. On the Kennedy property, lot 17, con. V, of Carlow, an (X-currence of magnetite has lately been discovere iiMix-rly, a strotiK Uit very irregular iiuiKiuti.: aitt.Kti..,' in-lr .ii.-s the |.n-s.MU-.- o! s,-vrr,il .l.Ma'lu- Miiall ..„• IxKlios. Tun small ..uan.p, ot m.i^nvUH- and sov.-ral i*olai..l cxi.u,UH> ..I Willi.' .lyMalliii. lim.-,tM,i.' ai>,l aiii!.liil...lu.'. appatfiUly lu- fliisions ill a laixi- Kiaiiii. iiitniMvr, win; '.I.MTvr.l on tins lot. Lot AO. Con. XIII, Dunftiinnon. On tlu- south -i,l,. ,A a ridvto running ta-t and wosi on lot M). mn. XIII of DuPKan-ion, an ..pt-n-iut lias Invn niadi' cxiioMnv; a co.irsf gramutl Kraiiif, with ^.HiH- niai;iiffite. Tli.- ore i^ of kihkI i-hararior as !,l,osvn hy Vlu' lollowiiiK aii.ily.Ms. Iml tlur t-xt.-nt of the oru ImkIv h very I'miteil. the niamu-tir attraction heiiiR v.ry weak only a tew feet from the exposure of maijnctite. Ip,„ (I'.l Cm per cent. Silica;::::::; i-^o ;; I'hosphoru* "*2 Sulphur <» "II k .N*, Bow Lake Iron Ore Deposit. On the north half of lot 21, con. X. and on thes.nith half of lot 21, coti. XI township ol Faraday, some (Hcurrences of ma^;iietue have been l.nm.l. The tirniHiiies are situated on the west side of Hr.w lake, and can easily l)e real hcd Ly wagon road from the villaRe of Bancroft, a .listance of about (i miles. The riM k formation of the area is to a great extent made up ul a coarse Brained red granite, the chief constituents of which are a pmk tel.lspar with some hornl.lende and (luartz. Other ro.ks of the area are crystalline linuMone and amphibolites, forming smalle .r larger inclusions m the granite. The magnetii.', a^so^i.ltod with mica, chlorite, aipatite, and ii<.rnblende, occurs along the contact of the linu stone with tlie granite. It wiU be seen from the .iccompanying map that there exisis a rather strong nia-.-netic field, along the west slope of a hill trending north and suiith on ot 21, con XI. Several open-cuts ;ind lest pits have been made a.ong the lino but tione of these workings has revealed any ore body ot sulticient size to be of economic importance. .An a v, rage sample of the ore g.-ive the tolluw- ing analjsis: - Iron "'1'^ percent. Silica ■'j:'^ :: F'hosphorus 1 "* S,,ipi,,.f. 070 Farther south on both sides of the line between concessions X and XT, a strong but irregular attraction is found in sevoral places. * -^J*. wfs^m ;;jfrii'K-<<''^ 23 CHAPTER VI. DESCRIPTION OF TITANIFEROUS MAGNETITE OCCURRENCES. Several small deposits of titaniferous magnetite are found in the district, associated with the gahbro-intrusives. The character of these deposits, their lack of definite form, and the manner in which they gradually shade into the normal gaV)bro, show that they are only a phase of the rock, in which the titaniferous magnetite, usually scattered through in small grains, is locally concentrated. The higli percentage of titanium, together with the irregular extent of these deposits, render them of little economic importance. The Horton Mine. On lot 57, west of Hastings road, Tudor township, some stripping and trenching has been done on some more deposits of magnetite, which occur at the western end of the lot near the boundary line between the townships of Lake and Tudor. The magnetite occurs in a gabbro-diorite into which it seems to gradu- ally merge. An average sample taken by the writer ga\e tiie following analysis: — Insoluble 2900 percent. Iron 40 -GO Phosphorus 0020 Sulphur 006 Titanium 10 00 Lot 17, Con. XI, Lake. On lot 17, con. XI, of Lake township, some prospecting has been done on several small patclics of magnetite associated with gabbro-diorite. An average sample taken from one of the workings gave the following analy- sis:— Insoluble 25'2.5 per cent. Iron 52-40 Phosphorus 0.012 Sulphur 0034 |; Titanium 15 '31 Lots 9 and 10, Con. XV, WoIIaston. On lots 9 and 10, con. XV, of WoUaston, a large intrusion of gabbro diorite occurs with some magnetite disseminated through the rock. ^ CANADA DEPARTMENT OF MINES MINES BRANCH Hon. Louis Coderre, Minister; A. P. Low. LL.D. Deputy Minister; Eugene Haanel, Ph.D., Director. REPORTS AND MAPS OF ECONOMIC INTEREST PUBLISHED BY THE MINES BRANCH REPORTS. 1. Mining Conditions in the Klondike, Yukon. Report on — by Eugene Haanel. Pli.D.. 1092. 2. Great Landslide ai Frank. Alta. Report on— by R. G. McConnell and R. W. Brock. M.A., 19""" of print). (Out 8. 9. 10. U. 12. 16. 17. 18. 19. 20. Investigation of tlie different electro-thermic processes for the s.rielting of iron ores, and the making of ste<'l. in operation in Europe, report of Special Commission — by Dr. Haanel, iy04. (Out of print.) Rapport de la Commission nommee pour ^tudier 'ta divers precede filectro-thermiques pour la rMuc- tion do- minerals de for et la fabrication de I'acier employes en Europe — b\- Dr. Haanel. (French Edition). 190.5. (Out of print.) On the location and examination of magnetic ore deposits by magnetometric measurements — by Or Haanel. 1U04. Limestones, and the Lime Industry of Manitoba. Preliminary Report on — by J. VV. Wells, 1905. (Out of print.) Clays and Shales of Manitoba: Their Industrial \'alue. Preliminary Report on — by J. \\\ Wells, 1905 (Out of print.) Hydraulic Cements (Raw Materials )in Manitoba. Manufacture and Uses of. Preliminary Report on — by J. W. Wells. lUO,",. (Out of print.) Mica: Its Occurrence. Exploitation, and Uses — by Fritz Cirkcl. M.E.. 1905. (Out of print: see No. US). Asbestos: Its Occurrence. Exploitation, and Uses — by Kiitz Cirkel. 190o. (Out of print: see No. 69), Zinc Resources of British Cclumbia and the Conditions affecting their Exploitjit^on. Report of the Commission appointed to investigate — by W. K. Ingalls. 1905. (Out of print.) •Experiments made at Sault Ste. Marie, under Government auspices, in the smelting of Canadian iron ores by the electro-thermic process. Final Report on— by Dr. Haanel. 1007. (Out of piint.) Mines of the Silver-Cobalt Ores of the Cobalt district: Their Present and Prospective Output on — by Dr. Haanel. 1907. (Out ot print.) Report Graphite: Its Properties. Occurrence, Refining, and Uses — by Fritz Cirkel, 1907. (Out of print.) Peat and Lignite: Their Manufacture and Uses in Europe — by Erik Nystrom, M.E., 1908. (Out of print.) Iron Ore Deposits of Nova Scotia. Report on (Part I) — by Dr. J. E. Woodman. *A few copies of the Preliminary Report, 1906, are itlll available. I 21. summary Report of Mine, Branch. 1907-8. (Out of print.) .,. .on 0« Depo.it. of ThunCe. Bav an. Kainv Hive. .i.tHct. Report „n_t. P. ..... M-E^ 23. Iron ore Depo.t.. Mon. the Ottawa (Quebec side, and Gatineau nver.. Re,.rt on-by Fr.u (Out of print.) 24. General Report on the Mining and Metallurgical Indu.trie. of Canada. liWT-S. 25. The Tungsten Ores of Canada. Report on-by Ur. T. L. Walicer. 26. The Mineral Production of Canada, 1906. Annual ^J^-^^f^-.^'^ton^^^^^^^^^ 26a French transition: TheMinera.Product.onofCanada.1900. Annual Report y 27 The Mineral Production of Canada, 1907. Preliminary Report on-by John McLe.sh. 27a tL mL. production of Canada, 190. Preliminary Report on-by John McUi.h. (Out of pHnU 28. summary Report of Mine, Branch. 190.. (Out of print.) Nystrom.andA.Anrep, I'catbxpeti. 32. Investigation of Electric Shaft Furnace. Sweden. Report on-by Dr. Haanel „. iron ore Deposits of Vancouver and Texada islands. Re^rt on-by L. - ■-'■;~;'^- . Report on the Bituminous or pi,.ha,es of New Bruns.icU and Nova Scot.a. also on the Od-shl. dustry of Scotland— by Dr. R. w. tus. .,,.,. 38 The Mineral Production of Canada. 1907 and 1908. Annual Report on-by John McLe.sh No.K.-r., /o»»-». Pr..».-..,y B.U,,ns ... .uU..a ,r.o, ,o .». .-»« »/ "..'»—' Rtporlfor laOi-S. 31. Production of Cement in Canada, 1908. (Out of print.) 42 Production of Iron and Steel in Canada during the Calendar Year. 1907 and 1908. 43 Production of Chromite in Canada during the Calendar Years 1907 and 1908. 44. Production o, Asbestos in Canada, during the Calendar Years 1907 and 1908 45 Production of Coal. CoUe, and Pea. in Canada, during the Calendar ^ears 1907 and .908. (Out of prmt). ^^^ ^^,^^_j^^ ^.^.^„ ,507 and 1908. 40. Production of Natural Gas ana Paroleummv.an . .„,3,o,i,. of the Department of 59 Chemical Analyses of Spedal Economic ^^^r^-^^l^^y^ct ^^T^^^^y^ the Commercial Sll'JirJsl^i'.^PPa^r Lrthe'lnLb'sV^ ^ 'c.-shaies-by H. A. Lever.n. Ch. E., Schedule of Charges lor Chen.ical Analyses and Assays. ■ , /■ „,rf, imm Preliminary Report on— by John Mcbeisn. 62 Mineral Production of Canada, l.'U-'- freiinuna y i~ I ;ir «s" r ir M^ritiac county. Quebec. Builetin No. .-by Einar Undeman. .:.ec:tr^-Jt:gs;^^o,,^^^^ .. Chr::r::tr;s^r:ce. .p,oitat.o„.Mi..ing, and Uses. Re.rt on-by Frit. Or.,. (Second Edition, LnUrgcd.) ,„ ^„i,^ ;, appended Mr. Alf. uie. ber 2 r. mo.s-translatiou by Mr. A. ''^ „'l';, JJ- i'*'„', " Ekelund Process for tlie Manufacture SI. Frel}": J:l Chry«,t..e.Asbe.tos, lis Occurrence, Exploitation, MiUin. and Uses: Re^n o»- ,2. Ma^nrCc^;i^:ation Experiments. BuUetin No. ^ ^^ ^■^^;;^;^^^^ ,, ,„„,„,.,a at ^- - Slif llS-.^Ii^nJiS' t^ ^Si^lt -^••^Sil::>^o;;e;;='^iaport on-by J. «. Por... F M n Sc R. J- Durlev. Ma.K.. and " hts E-M" "■^:'(,';-.i'\„...)iin„ .inH Coking Testa. Vol 11— Boilvr and Gas froducer Teaui. Vol. Ill—, '^'coaUVashing Test, and Diagrams. Vol. IV— Aiip'-n.lix II H.iilfr T IS und Diagrams. Vol. \' - At>i«"ndix t li I'roducer Tests and Diagrama. Vol. VI— Appendix IV Cokini: Tests. Api»endix V Cliemical Tests. Gypsum Dpposits of the Maritime Provinces of Cauada—lncluding the Magdalen Ktlands. by W. F. Jennison, M.E. (Out of print.) Report on— 84, 88. The Mineral Production of Canada. 1909. Annual Rep/>rt on—by John McLei«— by A. C Lane. Ph.D., with Intro- 118. Mica: Its Occurrence, Exploitation, and Uses. Report on -by Hugh S. de Schniid, M.E, 142. Summary Report of Mines Branch, 1911. 143. The Mineral Production of Canada, 1910. Annual Report on — by John McLei=h. Note. — The follfrwing preliminary Bulletins itere published prior to the issuance of the Annual Report for igio. 114. Production of Cement. Lime, Clay Products, Stone, and other Structural MateriaU in Canada 1910. (Out of print.) U.i. Production of Iron and Steel in Canada during the Calendar Year 1910. (Out of print.) 116. Production of Coal and Coke in Canada during the Calendar Year 1910. (Out of print.) 117. General Summari* of the Mineral Production of Canada during the Calendar Year 1910. (Out of print.) 145. Magnetic Iron Sands of Natashkwan. Saguenay county. Que. Report on — by Geo. C. Mackenzie. 150. The Mineral Production of Canada, 1911. Preliminary Report on— by John McLeish. (Out of print.) 151. Investigation of the Peat Bogs and Peat Industry of Canada. 1910-11. Bulletin No. 8 — by A. Anrep. 154. The Utilization of Peat Fuel for the Production of Power, being a record of experiments conducted at the Fuel TestinK Station. Ottawa, 1910-11. Report on— by E. F. Ilaanel. B.Sc. 156. French translation: The Tungsten Ores of Canada. Report on — by Dr. T. L. Walker. 167. Pyrites in Canada: Its Occurrence. Exploitation, Dressing, and Uses. Report on — by A. W. G. Wilson. 170. The Nickel Industry : with Special Reference to the Sudbury region, Ont. Report on — by Prol. A. P. Coleman. Ph.D. .„. M..n«.. occurence. ,.o„, U. CenU.. OnuHo ...wav Re^-n ^ , u a.-n. «7. F„nch transition: Mo.vbd.nun, Ore. o. Canada. K.:.r. on-bv Dr. T. U %Va^ „8 r„nchtra„.a,.on: P«. and U.nUe., The. Manufacture and U.. i- Europ-bv Eri. Nv..ro-. ...Xbe:;rroduet,ono,Canadadur..becaK.ndar.ar.n..nnua.«e.rton-b.,^^^^^^ R.po,t!oy i«/r. ^^^^^ g^^^^^^^^, ^^^„^,. ,„ canad. '«'du*;i^Tbrc"a^n^d'rj^MiT.'.'=&U?l'^byJohnMcUUb. .s/p^lctlon 0, Uon and St«. in Canada durin. tbe calendar .a. ,«n. BuUet.n on-bv .:m.ar. o. .. Minera. Production in Canada during tbe Cendar .ear .U. Buiietin on-bv John McLe..h. ^^^ .„, o.Her Me.a,. of Canada, duHn. ''^■Z'?^^^%°L?&n: ItL^i^yl- T. CartwH^ht. «0 The production of Coa, and Co.e in Canada durin. the Ca.endar vear ,0... Bui.et.n on-bv John ^, Prenchtltion: Craphite: U. Pro.rtic. Occurrence. HeBn.,. and U«-bv .it. Cir.e,. .»0. J • . r,.,,,!, 1B12 Preliminary Report on— by John McUish. 216. The Mineral Production of Canada. l«w- t-roumm. , 224. Summary Report of Mines Branch 1912. IS THE PRESS. TWrkriR No K' December W l^'V""?''] ,. Peat Probtem;" IWm describing the Ekelund Anrop. (Second K.lition enlarK^l.) 203. Building Stone, of Cana..-Vo.. U: Buiiding and Ornamental Stones o, the Maritime Provinces. Re- ^33...=:;tz;^rj^..^-"— ^^ MAPS. te Magnetometric S, ,vev. Vertical Intensity: Calabo.ie Mine, Bagot township. Renfrew county. OnuHo ' _by E. Nystrom. 1904. . r>_. j„ tl3. Magnetometric Survey of the Belmont Iron Mine.. Belmont township. Peterborough county. Ontario _bv B. F. Haauel. 190S. . „^„ , tl. Magnetometric Survey of the Wilbur mine. Lavant township. Lanark county. Ontano-bv B. F. Haanel. -Mrom^c^:,«tM- .tLConcessionVl. Mayo township. „a.ng.co^, «. « f Mer Bleue Peat Bog. Gloucester towr.shir, Carle.on county, and Cumberland township. "• ^"RSse"' c'^um?. OntiS^b^'Erik Nystrom. and A. Anrep. ^7 Survevof Alfred peat Bog.Alfred and Caledonia town,h.p..Pre,cottcounty.OnuHo^yEHkNynro«. and A. Anrep. '^'"•-J- 55^SSSl3t!;S:Trve"tL°^?^toVedlnde^ndentlyof report., hence can be procur«l .ep.- ratelv by applkants. »38. Survfy of Wflland Peat Bo«. Wainflftt »nd Humbtritone townships. Welland county, Ofil»rt»— by Erik Nyitrom, and A. Anrep. •3» Survey oJ Newiniton Peat Bof . Osnabrook, Roxborough. and Cornwall townships, Stormont county, Ontario— by Erik Nystrom, and A. Anrep. •40. Survey of Perth Peat Bo«. Drummond township, Unark county, OnUrio-by Erik Nystrom. and A. Anrep. •41. Survey of Victori.1 Road Peat Bog. Bexley and Garden townships. Victoria county, Onurlo-by Erik Nystrom and A. Anrep. 48. Magnetometric Map of Iron Crown claim at Klaanch river, Vancouver island, B,C.-by Elnar Linde- man. 40. Mannetometric Map of Western Steel Iron claim, at Sechart, Vancouver island. B,C.-by Elnar Linde- man. SO. Vancouver island, B.C.— by Elnar Lindeman. 61. Iron Mines, Texada island. B.C.— by E. H. Shepherd. C.E. 62. Sketch Map of Bog Iron Ore Deposits, West Arm, Quatsino sound, Vancouver Island, B.C. •53. Iron Ore Occurrences. Ottawa and Pontiac counties. Quebec, 190*-by J. White and FriU Cirkel. t54. Iron Ore Occurrences, Argcnteuil county, Quebec, 190S— by Friti Cirkel. 167. The Productive Chrome Iron Ore District of Quebec— by FriU Cirkel. t60. Magnetometric Survey of the Bristol mine, Pontiac county Quebec— by Einar Lindeman. 61. Topographical Map of Bristol mine. Pontiac county. Quebec— by Einar Lindeman. trlic;il Iiitfn«lt> : "oehill and Jcnkini minn. WoMajton lownihip. llasiirs* county, Ontario — by K. Lmd-^raan. ltt!I. tItOa Geolojical Map. Cocliill ami Jcnklni inlnM, WollaKoii townihip, llattinx* county. Ont.irlo— by E. UiuTcnian. lUll. tl91. Mafnetometrlc Survey. Vtrtlcal Intenaity: Bfisemcr iron ore depoiitj. Mayo townihip. Ilaitlnia county. Ontario — by E. Lindcinan. 1911. tlWla licolotlcal Map, Bc' M' 2M° 4tf or Nf^'ative Intousiry^ m. 20° 40' 2(f 40° «<> Matirutif altrnrtinn urrtUrr Hum -HO' Coiuiant oflmtrunitni 1.0 H Mofinetic lUf H nalinn uhotu WWtat H. S. Bmmt, Chiaf L.H.a.Pw*m, ST. CHAR I.OT 19, TOWNSHIP ■▲■TiMei ONTj Scale tAit ■ Csniidn kRTMCNT OF MINES MINCa •NANCM Ma«,Mi(iitri« APlMT, l,LO.Dtlliliw lulruailT ^^^H MMftHMif aOrarrttaM grmUrr tkMt tUr SW tU) Hf aar Hf 4tf Ne^liTv Intsnsiry I i I i -aw 4er Iff - -Stf Con^ttuU of /njitrumstit -• 1.0 N U. M. BaiM, Cki>/ L. y. a. Pmtin, DrmufkUmm BELMO X TOWHI FITB] Sea t^m^ OKPAKTMKNT Or MINES M*Nt» ••*M«N KLMONT IRON MINK IA>T 19. CON. I TOWNSHIP or BSUIONT PBTBXBOXOUOH OODMTT ONTARIO Scale ■*•- MW to 1 Isek K. Umdmmm» l»ll A-ifd t» IT. H. Mommn I.KIiKNII i .- ,; * MlHulm imii hiittilinfm HaUwt^tm TX ! »tid0^ I C^ ! .'iirippiiuts s Tmch— DIFARTM Mm MA3NKTOMrrmC MAP UtOBlID RsMhIW MAnuB^r SO' - mr tr - ^ tr - -w «r - -»*• ur - -••r 1.0 N «.s.ariM,cu^ k fl> '• npf#a, A BAKl LOT IS. ■aani Ol ^■■■■m »CPAIITMgNT OP MINK9 ■■MtM Wm— t .fll.tL.tl— ■»■■ BAKXR MINB LOT 1«. OOK. ZTIII T<-wB««iy or nrBoa OMTA.aiO >. riiitiiiiii Mil 4aiiWI*0.e.ai rfS^i KICB^XSV'TK* (Tn MAGNETOMETRIC MAP DEPARTME MINCI Hon HoBfHi RooiPs.MiNiSTt fuocNC Haak iiniliw* Uil**itaiiv N«-(»»tiiv«> lut^nailv w «• 2*r 2«* -*»" H If HiiMr ' 'Am/ finiwfA'i RIDOE IRt>! LUTM 17 AND iH, ros i TOW!M.HHI»i BAMTI O (Tnu^tDa RTMENT OF MINES MINES BRANCH p». Minister v P Low, LLO.OfPUTr Miniitck lOfNt HA»m "m D OmccTOB p6 .,r> \ _, r ^ ( 1 f \\ '<^ 1 \ ) N^' H'MttL tmii huiiMitOM •<>«M N (M^E DEPOSITS IM, rOS 111 «ll IJ)T!» 18 i.VD 17 CON. II VlMMRIf tt wnt.l.AfJTCtK HA«TIN i^ COCXTY O.N r* -fio .Surinn*' 6* f-. LtndmMiii 1.1// Lit 'm mmm mm MiaiOCOfY MSOIUTION TEST CHART (ANSI ond ISO TEST CHART No. 2) 1.0 I.I Hi 1^ 2.0 1^ 1 40 1.8 A /APPLIED IM/1GE I SS*^ '653 Eost Mom Slr«t S f.a Rochester. N«* York U609 USA ■^S {^'6) *82 - 0300 - Phone ^S (^'S) 2S8 - 5989 - Fo* MAGNETOMETRIC MAP i.k<;i:m> hfttivuftniif iitirn itt thr vtiuuit nrtitiriftn- intrti.titv Noj^niivf Uit«-iiHiiv L ' L. Cnnndn DEPARTMENT OF MINE N^lNES BRANCH Hon RoBFRi Hoglh , V nistcr . A P Low LL D . Df putv EuGf. Haanel PhD . Director ^^p DEPARTMENT OF MINES MINES BRANCH Hon Ro. . iGtHs.Mr. v « A P Low LL D . Deputy MiNrsTER Eugene ■■»»-.fl PmD.D ector m:(;kni) /itMltln lUIti hitliJttU/A t'lutirr intiltt ttifl I III Ulf ■fy /{f/h-^nrr /*.*.*/.* Ihntmmil tli^il Itttlf Q_ J Oftfti en/.* tifitj Tr.ll ftti.t ' — f— /*(/.? tillrti with %^nt*'f i*'""] Ctmttmr.t. inUrvni Iff fe^t --- "'' i h'/rrrttittns' tihtt\f Jtea l^vel N«'\;iilivi« littiMiNilv Ht Mnorii'lir .illitivti„f, ,ii-f„i,;- than -tifj t'.tnjthuif .it hi. if rum. Ill | H Miionrli.- ,1.;'lin,itn,i\ ,th>>ut liV Wrj^t H. E. Baine, Chief Draught ttman L. H. S. Pereira, DrauahiMman M^rittiMMaitaMrtriAi mtm ( Jatauflity 20' 40' .W iv ! 5/r - - n(t t'.4*n*tnnt «/' ln*trurtiMjxt - 1.0 H Mn4tnetif U^.rltnnb^n ahout II ' Went €) DEPARTMtl MINI Hot RoBfui Roci M M N ir^ dnnadn •ARTMENT OF MINES MINRt BMANCH ^ooins.MiNit'O A P Lew 1 L D . OcruTv MiNiartR E0«tNt H».>.l PHOn.xtCTOB t i.k<:kni» [--v] l^J f ^- - I Mii/> •t\v« llliiilll I t'UxUtil tnim'iiy L .- _ . • Duunond driJI AaU i-^f^-*- Swamps I ~r^ £UraMUfns ai>ove sen Uvf4 Mut* diunps cn 4V nr a" «• *»• **• ■ur 2ir nf ■uf mf Iron Ore DepoI LOT 1. CON. \ II. Towns II HAS'l IN< ON' Scair ».T t»o too mmmm^^^^. Deposits at Bessemer ►N. VII. ii, 3, 4 AND 5. CON. VI ►M^NSHip OF Mayo HASTINGS COUNTY OINTARIO Seal*. tA. 200 Teet to 1 Inch zoo JOO 400 Ha, II. I K I K. A »ngte %00 600 Si^'fet^ir^'"- -e-f r— " -■J,^^.. T ■!>-.— »^ Wn.. -1-1 J ■f-T.^TTT^- — NO. 1 9 1 Wairneli}r'tftrn- Survey H. FrirhtUt ■ l!H)tt E LtruUnuin - lyii Topography f. Limteman Ifltl Aan^le't f>u W. M .Worn-.., Wrv«t*r /•••<*l« ti^*'ti0^ tmmm^t I 1 ftrn4tf^» Ut n m t mmt t *tit4S h-t* f^"> f»M#(iH#4 i#itort««/ httm04 --r :^r..-—^ CauaDa I.KC.KNl) nuianfli*' nttrn.ftt}' ^^^^^H AAi|*?nWJ> attmf^\*n (ft'^at^'r than fiO" hrX^ 5lt 40° 20' or 6U" M' 40- DEPARTMENT OF MINES MINES BRANCH MAGNETOMETRIC MAP Hon. Robert RoctRi.M •. jter. A P, Low, LLD, Deputy Minister EuGEN' ^«ANEL. Ph.D. Director Nf*i^tiw Tnteuflitv hfitt - 2fl' 20'' ■44)' I'*' DEPARTMENT OF MINES MINES EPANCH KoHKRr Rogers. MiNil't" ''■, ? Low LL D . Deputy Minister Eugene Hjanel ^ ■■ D Director i,k(;kxi) HiMiiim tuid huihUntfA ' T I ihmer pa/ltJV tuul Lot lil Hfferrtirr fimtl^ JZC Hriiliirtr [^ t^Mwt- ^^"^- *- Swamps I /'^J Conluiir.i.inlti-v/' In/ttrutnftit 1.0 H H. E. Baine. Chief Drauffhttman L. H.S. Per^ira, Drau(ihttman ittifllMMHrfta^iMAl Mil Rankin. Childs and Stephens iron ore Deposits L.OTS lO. I!. 12 AND 13, Con. IX TOWNSHIP OF MAYO HASTINGS COUNTY ONTARIO S.J;.' lAo- too' lo I Inch [STEPHENS IRON ORE DEPOSITS . 12 AAD 13. Con. IX rSHIF OF MAYO |SiL\r.S COUNTY ONTARIO SuTvtyed 6|/ H. FrtcheHr U E, Lindeman - U AuuUdby II V.J/i SckIf ,i- .,„■ |„ , Inch >e]/eti by 'rtchfUe f9f)S indeman - I!* It ■ fty *l tf. Momnon '■>. (j. thi'lakvr NO. 192 'i t'nttief fMt/tl.»i*iv«» lult'iiNiiv /.w« 50 N«'t^'i»iivi> liiii-iiHit V MAGNETOMETRIC MAP DEPARTK Hon. Robert RooERS.Ml^ EuocNi (Canada »ARTMENT OF MINES MINES »RANCH ooeRs.MtNiSTER. A P Low. LL D . Dcputy Ministcm EuOtNE HAANf L.PH,D.,DmtCTO« LK(;knt) L— — -1-1---^ "*r j Commr pw9tfr tinti /.»*r ic/t#« I C .../j j Strtppintfji \ -ifcJ -*■ Swamp ^ CvnUiur.i. ini^rvui If) f^^f N«'l**alivi' liili'iiMitv N» f'»tnmhitit lit' litMtrutnmnl I H H. S. Baine, ChUf DrattgHlaman L. H. S. Ptreira, Dmui/lUaman IRON Ol LOTS 1«. 17 C mrnggmgrnj^^^^ •■i )N ORE DEPOSITS ITS 16. 17. 18. CON. V AND VI n^RI.OW TOWNIIIIII> ONTARIO St a.le i^ - tno' to l Inch Survty«d by B. //indnuui Wll AuiMed by W.M. MomnHi NO. 193 I /".'Ir^iltifftM nA».t#- tjF¥rl of FrttMer Lakr Mmr t/u/fytjr !1*g MAONCTOMSTRIC MAP OfPA»T.M r or MINtS I.KIiKMl iiMilivr IntruMiiv if Kl' N^-liHlivp lulflmilv ;« *< *> »**■ /. H .1 /■•rnra. KivivU BOW LAKE IKON <)KE DEPOSITS LOT Jl I <»\S. X AND XI TOWNSHIl' OK KAHADAY HAS! I\«JS ( OUNTV «>\TAK10 tt^Ht.U .U,.i hu,l,i, ■ 'tuT i-iimlM xMi/ I «l ttttf C t'(»'M tM»* lWt«f /fJI* !••(.« ■ d^jiy .»/»«r lOfi^T^Ji MicRocory rkoiution tbt chart (ANSI and ISO TEST CHART No. 2) ^ ^jPPUED IM/1GE '653 EasI Moin stre«l 716) «82 - OMO - Phon. (716) 288-5989 - Fo. In -"■^ GEOLOGICAL MAP w P^ r — .-_. I . LKGKND l^rifteovered area Ai-fa, wtthiji wfurh A/offnchtf t^ hJeeJv tn nccxtr, ijidic^xt^^i bv Mafjftetomftrif 4*i*Jrvfy tnuL caruflomtTair lyUtritr, (.Irch^an.) f'ry^taUute Ixirieatimr-, chlorite etrjuat Striate nnti tiif* r C H Canafta DEPARTMENT OF MINES MINES BRANCH Hon. Robebt Rogers.Minister . A P Lo^. LLD. Deputy Minister Eugene HAANEL.PH.D.DiRtcTOR H O LAKE LKr.KNO f'—-:-^. — ^ Rimtiu anii biuliUitii/i O ItianumJ .It-ill hole i C Oliri, rut., „„,l /•,.,, ^„,, ; -*. -* Swatnif.r V*!^' f)>t*tonrM.intfrvni lit ti'rt Mmr ttumpa lh„r,t, lArrh,mn Cnmtaihrr bmrMfanr, Porplyyritie homUmilr and ^^■^\ StriJte nnrt ittft H. E. Baine, Ckitf DraugMsman L. H. S. Pereira, Draughtitman BLAIRTON IRON Mil LOT 8, CON. I TOWNSHIP OP BELUONl PKTBRBOROUOH COUNTT ONTARIO Scale lAo- 20CV lo i Inch >N MINE . I BLMONT 3017NTT » 1 Inch W2' w Gmloffy by B. Lind9man 19 tl NO. 185A —*..*-* Swt$tnft,t ^1^ "^ t'ttttt4»ur.t ttiUrvttl ittfi'ft Mtne fliitufKv *0O M>o €nt Ur%fttjB(vtt/>rd area OiUrrop of Ma^jnmtUt eOKMSQQ Drittcaverrd are^ wdAxn whirK y^^^m Magn^jbte ui bkeir to occur, indicatetl '//'//ffft, bv Jttufn^ametrtr Survey (Arrhmmv) < A^ ■^ i [ >< >^< ( Dian/4 1_ ^ > A I E 7~. ' ^ /* Crfaiaihmr bmeatonr \y *>^ AsrpJ^rittc achiat GEOLOGICAL MAP OCPARTMEN MINK H. B. Bain; Chitf Dm,glu,man L. H. S. Pertira, Drauthltrnm BELMONT I] LOT IB, < TOWNSHIP OJ PCTXRBORODt ONTA] Scale 1^ - sw m Canada ^RTMCNT or MINES MM.Mmrltl* «»!.»« 110. Ot»M»v UmKria (u«l«a HaamIl Pm DiMMTWi -eso. )NT IRON MINE LOT IB, CON. I SHIP OF BELHONT ERBOROtroH COUNTT ONTARIO Ale 1^ - soo' to L Inch S. Undtmm 1911 Ml ! -0- i.K<;i.\i» n.HuU ,n„l l,„il,l,„„t lirHrn-tifr fmttl/t -A ;T T I hruli).;^ i*Mnttn\,t lUtU hitlr 0\_-^ I Oft^U rut.* Swaifip.j Tf^fivhfit Mine dumps Cana OCPARTMKNT MIMC* •• Ha«. nMtar ll*Miift.MiMiiri« A I.KOKNU hrtffnivrr^ri nrm 99SK99S9 by MtffntOammtr^r Svrrm \ >< >"< Ouirilr ~ I y\\ Vnatatlmr tomntoiu- lArrhmm) H. K. Bain; Cl^itf DniitlUmum L. H. a. Pttin: DnutlUtman ST. charl: LOT 10. C TOWNSHIP C HABTINOS I ONTAI Scale tAft - zoo' Canada TMCNT or MINCt I,K(iKNI> KtHttim luii 'ittfM LJ tUt^r^ftte pt»mtM f I ikp^n riit.i ^1 '■ Strippittftn ■f. *•-*. SwaivipM CorUoura. iniervai f*> ^## Mittr liu/np.v ;harle8 mine >T 10. CON. XI SHIP OF TDDOR ■TIMOS COCMTT ONTARIO p lAft - znn- to I IiuJl Omioty bu K. lAndtman 1911 OCPAH HoM RoiiNt H^^uti GEOLOGICAL MAP Itri/'ti-it r-rrii nrrv Oii/tritii !•/' M'lifn^lilr yiatjitrlttr i« hJrrH tn nmir. t mh».h H.K Ha\Hi\CKi*f t)niuvhlairtan I.. If S Perftrti, iJruuti/Uimtai itoMriWii mk^ttaM €nnnbn DEPARTMENT Of MINKS MlNKft SWANCH C _^ "'"■" •'•"• •""* T>-^i f'U., I ^Cjjpjaki Mitif liuftlfKI KAKKR MINE LOT IM. CON. XYIII TO^VNMHIP or TITDOH HASTINGS COUNTY ONTARIO Si-nlr lAn ■ simv (n i Iniii 'ifotagy by ti. Lindrman 1911 rui/ .»- .rt»--* I L. k^ ■T«*W«IBI»T GEOLOGICAL MAP l-K(;t;M) Ih'ifh'ihvrrfii nrffi (hitrrttn of Mmfnfhtr (ArrhtF/i T; v;f.T; ^ 1'^ \ '^ /I CrTT^anzjw itj..i.-,ttn t^rhtjSt.s aiiii ajnpfnhnhtrs Strike 'in ft till! DEPARTMENT OF M I N e| MINES BRANCH Hon. Robert Rooirs.Mims ^. A.P Low. LL D . Deput^ Eugene Ha. ;l. Ph.D.. Director Cnnnfta DEPARTMENT OF MINES MINES BRANCH iHtRi RootRS.MiNiSTEF '^ Low, LL D , Deputy MiNisTtn EuotNt Haani h D .Director i.i:(;i'.Ni) /,'.„!, /,, ,„„/ I.Uli.l,, ('t>ttfl [>lt.'.l.\ Rri:-nni:- ji,:sl.'t ».lll,.„X ../ v., / ( NO. 190A Otology bv b', Lindeman 1911 OEOLOGICAL MAP I.KOKNU OttttTop at Mtutnttttf' ^^^«j l*intU:*ivrr,^ area wiMin wfarh 'yr/Ar/Zr/i bv Mafjnetomfttrtr .SurY^ OymtmUmte kiM»tmv.mrhaMm (ArrKmms,! J mtd. mm^hthotOnt iir-antte aiuL - 1 : ^--"^ Strike and dtp iffroiuif^nnjni DEPARTMENT OF Mil MINt« U-tNCH Mow HoBrnT HiKiiMi M>»» s f - Cnnnda JEPARTMENT OF MINES MINKS BWANC [)f PU'V M'klj t ^t M I.I.I.I.Ml /.•...„/, ,„„/ i.,„,,i.„.„ O AV/rir,,., ,..«>,. ■*— / i."..!/.'./ /,,(«,-«,,. / "Z*^*! '"«/"«/. ifUTX.iJ litl^^, Minf ihuiutM 1 i Itrt/'it*t*^t^/ Mrw wdAifi wAtrA mt*4 «*fM^AfA«Alf« fitmHiie ami mrmiut^gn^um ^,^^ Sfrtkm rnml ,^. L. H. a. Ptnim. Drmit0ktman Iron Ore Deposits a^ L.OT 1, CON. VII. -J. .{. 4 ANl] TO>VNSHll» OF M HASTINCiS COUNT ONTARIO S<'alr . i«Do 10 reet to 1 Inch| 30* Ore Deposits at Bessemer )T 1. COi\. VII. 2. 3. 4 AND 5. CON. VI Township of Mayo HASTINGS COUNTY ONTARIO 20O f Ti to I Inch too V. u 4flC SOS 600 ll..„„.,H.I .It'll ' *V,f. . ,,l, .,t,,l ir,l i„l , r'Z^ '"■■•' ""••" J r,,. . ... B. Iir. ■■ I'll! NC I91A ]|-JI.J Li I >. i . vmjia^BBsmr^R ■*» GEOLOGICAL MAP LKOEND Dnftr/ivnyrA area (htirrup of Modfn^Ue. hv jiaff nrtum^trtc Survey (jy^taJIuw bnu'Mtm^, ScJusUf /ArrJuKtov) and amphihohtam 1 I i ^.^^ Stttkr and thp m DEPARTMENT OF MINES MINEJS BRANCH i Hon, Robert Ror.tRs.MiN'U" A. P Low. LLD. Deputy Minister EuGENt H»iNtL. Ph.D. .Director (NT OF MINES lis BRANCH \\^'.ii A p Low. LL D . DtPi.TY Minister fc^EL '-H D.OlHtCTOP* Opan. euU tuul lift pUm ^^ Strifipingft I.KCKNU lH^tr0f¥9rr4 OtUff^p of MoMfn^ttiit- bv Staff nrtomf^rw Siurvm* j j Qrmuu and. jp-mfUi StnU^ nnti dip Otiiirop 4it' Mtttfn^'Utr ^JN ltrtJ'U'4»vrr*nt firr<» withm which h^ Ma, j^ I ri'V0ta//inr Ittnr^Mtun^ .Sthists ArrJuman.) an// lunphihftltte^ CI I Orm-iir ,Mnd *fr nnMte^ntuta StrxJi^ iitui tiift II E. Uainr, CMtf Dnuehltmun I H a Pernra. Draugkliimnn Rankin. Chilj)S and htephens Iron ore Deposits Lots lO. 11. 13 and 13. Con. IX TOWNSHIP OF MAYu HASTIXtiS COUNTY o>:fARio v.. .A'l znn- u. I Inch too w 'EPHENS IRON ORE DEPOSITS 12 A\D 13, Con. IX miJ' OF MAYO riNGS COUXTY ^NTVKIO freotaffy hy H. Lintitman tun > IrMii - 1 Li a.— j a M^fel^MiitoHft Hrl, •mr* i„tmtm \ (^. "^ I « < ^ (iranttrji apt/ pegmatite grid prqn JuimUk RTMENT OF MINES MINES BRANCH ts, Minister A. Plow. LL.D.DtPUTv Minister OENE HAANEL.PH.D.,DmCCTOR I.KflKNI* Hi^nda ftlili htultUtulft — "V \ t'ltnirf pn^l^ iiritl l.itt hitfM I, -' ^ Hrti't'^IU'r pttJtt/t < r ') i sii-if,,.. L^] (hittmp of MaanMsl^ Itr-iftrnvrrrd arrm wiiAin vAirA Grmmtea arul prgmaltte. (Arrhtrmn.) Miaa^ and, hornhlmde athimtjt StrAr ani dip H. a. Banu, CM*/ L. H. 3. Pmrtira, IRON LOTS 16. 1 T. rik mttM 1 tniiff paMtM iiiui i.t't hti' ■ !?LJ I Mine tiwttftM RON Ore deposits S 18. 17. 18, CON. VI *"» IiOT17 COW. ▼ CAILOW TOWNSHIP ONTARIO Scale 1^ ^""' *" ' '"'^ (Jmlogy 6y B. Undtman tBll NO. 193A OEPA MAGNETOMETRIC MAP I.KCKM) l.9fHivnttmif ti:if,t ttf thy vfrtifai nuionftir intrn,iit\ Pf»Bitrvp Futpnsiiv yfiit/riflif tH/riirlutii ifi-rnlrr than Citt '^- ~^' ^^ h^l« .V) fit) 40 m 4«" Xf»l>Hlivf» luteilNltV h^tw^rn (t 20° 5t>° ■jtr 40 .w tuf Mtttlli^tir uttn^ffinn timiter than - GO" Canada DEPARTMENT OF MINES MINCa •MANCH Konn Ro'.iat.MiNitTtii Af Lm. LLD.Di>utt Mmiiri* ^w«tNi HAAMfL PhD Dinccrv* 1 ■- -— --- j KfMutM tutti btuUimuM -- i Ret err nee ptmt/t Diantutui th-ilt hul^ C, ^. ^ \ "/"•" .»/ />//.v VtOtllft r /""'" j f'*'ftt*Hi/\9. i/Hervtii Iff left \— '' — ' J t.levations nbttve jtea ievel Mine tlutufKt •»» w tt' Nl'tj'illivf IllllMINIIV ■Jlt' ■Ut ■u> .'til Mitailrtif it//fiiftlttri iirriilrl- ihtin - fiO'' I'littnhint nl' /njftrttrnfll/ i H .\l,i.lii--li- il-;l,ii.iliiiii iihiiiil I.I' H'l-ml 1. E. Batno, Ckitf Dntuehttman L. H. 8. Ptrmra, DraugtUtman BLAIRT Is TOWNS P«TBH Si-ah mmr % i iihnmii a»jyj> ^ ii i ii w i h i i irt¥kirr»-h'fS'iitrrm''Aaixvcmi,t:' u « «jj ^wis- '.»^iBwnia' " ■*>« .' \, 'l^Htn D LAIRTON IRON MINE LOT 8. CON. I TOWNSHIP OF BKLUONT PKTEHBORODOH COUNTT* ONTARIO Scale *Aft • L'tw>- to I Inch !< lOO *0O SAO t^O " ^ ^ - - J _J I , ] '/ ^■y Surveyed by E. Lindenuin lyil Asuistett by W. M. Momnon <^ tit trrrin-*- fUHft/t : \.._ ^_, '. *>l»rn tiit.i unit Vf.^t /*i/.» Mtn*' tiutitft.f : i.ir^_:r22^^fe!qSl»JOa?L»fi--?!BBaa5J 1^