CIHM ICMH Microfiche Collection de Series microfiches (■Monographs) (monographles) Canadian Instituta for Historical Microraproductiont / tnstitut Canadian da microreproductions historiquas Techn'cal and Bibliographic Notes / Notes techniques et bibllographlques The Institute has attempted to obtain the best originai 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. D D D 2 D D D D D D Coloured covers / Couverture de couleur Covers damaged / Couverture endommag^ Covers restored and/or laminated / Couverture restaur^ et/ou pellicula Cover title missing / Le titre de couverture manque Coloured maps / Cartes g^ographiques en couleur Coloured ink (i.e. other than blue or black) / Encre de couleur (i.e. autre que bleue ou noire) Coloured plates and/or illustrations / 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 serrde peut causer de I'ombre ou de la distorsion le long oe la marge int^rieure. Blank leaves added during restorations may appear within the text. Whenever possible, these have been omitted from filming / Use peut que certaines pages blanches ajout^es lors d'une restauration apparaissent dans le texte, mais, lorsque cela 6tait possible, ces pages n'ont pas 6t^ f ilm^s. L'Institut a microfilm^ le meilleur exemplaire qu'il lui a 6X6 possible de se procurer. Les details de cet exem- plaire qui sont peut-dtre uniques du point de vue bibii- ographique, qui peuvent modifier une image reproduite, ou qui peuvent exiger une modifteation dans la m6tho- de normale de filmage sont indiqu6s ci-dessous. I I Coloured pages / Pages de couleur I I Pages damaged / Pages endommag6es □ Pages restored and/or laminated / Pages restaurtes et/ou pellicul6es Pages discoloured, stained or foxed / Pages d^olor^es, tachet^es ou piques I I Pages detached / Pages d6tach6es I >/} Showthrough / Transparence Quality of print varies / Quality in^gale de I'impression includes supplementary material / Comprend du materiel suppl^mentaire Pages wholly or partially obscured by en-ata slips, tissues, etc., have been refilmed to ensure the best possible image / Les pages totaiement ou partiellement obscurcies par un feuiliet d'errata, une pelure, etc., ont 6X6 film^s ^ nouveau de fapon h 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 filmtes deux fois afin d'obtenir la meilleure image possible. D D D a Additional comments / Commentaires suppl6mentaires: Various paglngs. Thla torn it filnMcl at tha raduction ratio chaekad balow / Ca documant aat filing au taux de rMuction Indlqu* ci-daaaoua. lOx 14x 18x 22x 26x 90x J 1 12x 16x 20x 24x 28x »9v Tht copy filmed h«ra has bean raproducad thanks to tha ganaroaity of: National Library of Canada L'axampiaira filmi fut raproduit grica k la g^ntrosit* da: Bibliotheque nationale du Canada Tha imagaa appaaring hara ara tha bast quality possibia considaring tha condition and lagibility of tha original copy and in kaaping with tha filming contract spacificationa. Original copias in printad papar covars ara fllmad baginning with tha front covar and anding on tha last paga with a printad or illustratad impraa- sion, or tha back covar whan appropriata. All othar original copiaa ara filmad baginning on tha first paga with a printad or illustratad impras- sion. and anding on tha last paga with a printad or illustratad improssion. Tha last racordad frama on aach microficha shall contain tha symbol «^ (moaning "CON* TINUED"). or tha symbol V (moaning "END"), whiehavar applias. Las imagas suivantas ont *ti raproduitas avac Is plus grand soin, compta tanu da la condition st da la nattati da l'axampiaira filmA, at sn conformity avac las conditions du contrat da filmaga. Laa axamplairas originaux dont la couvartura sn papiar ast ImprimAa sont filmis an commancant par la pramiar plat at tn tarminant soit par la darniira paga qui comporta una amprainta d'imprassion ou d'illustration. soit par Is tacond plat, salon la cas. Tous las autras axamplsiras originaux sont filmAs an commandant par la pramiOra paga qui comporta una amprainta d'impraasion ou d'illustration at an tsrminant par la darnlAra paga qui comporta una talia amprainta. Un doa symbolaa suivants tpparaitra sur la darniira imaga da ehaqua microfiche, salon la cas: la symbols ^-^ signifia "A SUIVRE". la symbols V signifia "FIN". Mapa. platas, charts, ate, may ba filmad at different reduction retios. Those too large to be entirely included in one exposure ere filmed beginning in the upper left hend corner, left to right end top to bottom, as many frames as required. The following diegrems illustrste the method: Les cartea, planches, tableeux, etc., peuvent dtre film*s A des taux da reduction difftrants. Lorsque le document est trop grand pour Atra raproduit en un soul clichi. il est film* A partir da Tangle supArieur geuche, do geuche A droits, et do haut en bas, en prenant la nombre d'imeges nicessaire. Les diegremmes suivents illustrent le mOthode. 1 2 3 12 3 4 5 6 ••aocory rbowtion tbt chart lANSI and ISO TEST CHART No 21 1^ 136 ■ 75 1.8 ^«^ A APPLIED IIVHGE :ay- '653 East Ma.n Street p^S Rochester, NeloKi<'al Survey, Department of Mine«. SiH, — I heg hiTiwitli In *iiliinil a ri'port un an exploration aeDss tlie Araokcn/.ic nupiintaiii'i in the Yukon, ami North WVst Tcrritoric-i. TIk; report i» aeemn-'auieil liv a iiuip an '" Cliinntc 22 I'auiia 2* I'lir tittdf 2B V»r>-^'< » Tiaii-|iiirtatioii 2" r,..„lc,i,.y- - rjpfipral fU'^cription •»! Kork f(iiniati"iii« ami j;y 47 Index SI ILM'STRATIONS. j piinrnnBii'iis. riatc I. Wolf cafton, I'plly river Froutif>pirce II. Ross river, below rapi Oravel river from Mt. Sekwi ".. .18 " XIII. Sekwi canon, carved in Sil' ■ limestone ,38 " XIV. Mountains of the .'sayunei .^e, .N'at'a river »» " XV. Mount Helthore, and Shezai cafion, Uravil rivi'r.. .. 44 " XVI. Valley of Oravel river, and Tigonankweine rang.', above mouth of Twitya river 46 " XVII. Cliffs of Or.lovician sandstone, overlyinir a sill of diabase, slopes of Mount F.duni, Oravel river.. .. 46 " XVIII. Oravel river flowing through foothills in Markeniie valley 4H " XIX. .Ti'iiitiiiri of Oravel river with the Mackenzie (f innn. i!,f..i.. Yukon. Mill, '.f IN i.nd Oravel A UKCoNNAISSANCE ACROSS THE MACKENZIK MOINTAINS UN TIIK PELLY. ROSS, AM> CRAVEL RIVERS ■T .losKPii Kkki.k. INTBODUCTION. The prt'iient report is based on the results of invent ipat ions made during a portion of thf years liK)T-», in the niountiiin rt'Ki'i'i lying Ictwivn the Telly and ilackenzie rivers. Since 1897— the year following the diiy various members of the Ceoloxical Survey. This work has, hitherto. been confined principally to the areas where aetive mining was in operation, and these have been described more or less in detail. Owing to reports brought in from year to year by prospectors and others concerning minerals in the outlying districts, a more extended knowledge of the territory- sec.n<41!l l'. 1-' hia^rain nf Mnniitaiii S\>ti'lii> in \i'rtli\\H..tfMi CiUiitfla. ;/ MACKENZIE MOUNTAINS, YUKON ir 1 Two of the well-known topographic types that exist in the better known southern portion of the Cordillera have their nortliern counterpart in this region. Tl\e ooutitry of coir.puratively low relief bordering the Lewos and Yukon rivers, to which the name Yukon Plateau has been appli'jii ciirrcsiKiiid:* in position and topography to the Interior Plateau region of British Columbia. The higher and more rujr>{cd mountains to the east, which form the wutiT-parting betwaen the upper iviard and Yukon on one side, and the main ilarkciizie river on the other side, represent the north- western continuation of the Kocky mountains proper. The name Mackenzie moun; ilns is given to this portion of the system. The ilaekenzio mountains appear to be well defined; their axis is crescentie, the southern point lying in the valley of the Liard river, and the northwestern extremity reaching the lowland between the Yukon and Purcupine rivers. It is the greatest mountain group in Canada, and appears to consist of two ranges, an older western range, against the eastern edges of which a newer range has been piled. The names Selwj-n range and Ogilvie range have been appliey a belt of plateau country — rather higher in elevation than the Yiikon plateau— which extends south ard from the Pelly river, embracing the upper Liard and the I ances rivers. There is not siifficient knowledge at present concerning these mountains, to state their relationship to the plateau or the main ridge with any degree of certainty. Xaokeniie Xonntaint. The high, rugged mountains, farther up the streams, east of the flanking groups, and including the divide, present a fairly massive front, with no important lowland oreas breaking their continuity. The crest line of these mountains is uneven both in course and in profile, for included within them are groups of mountains of a more subdued type, and many wide, branching valleys, that are trenched well back to the main divide. The structure is charac- terized by folding, genurally on a broad scale, which has thrown the strata into a series of anticlines and synclinea; but the folding is sometimes close, and in certain cases the folds appear to be over- turned and overthrust. Many structural details, however, are con- cealed by the easy, well-wooded v ey slopes, but the outcrops for long distances on the rivers often show steeply-inclined beds of th" same kind repeated at intervcls. The topographic features are governed to some extent by the geology, for although the main drainage ways, as adjusted at present, cut across hard and soft strata alike, many of the wide valleys are carved out of the soft strata, while the higher ridges and peaks are formed of the uptilted hard beds. The highest peaks and the ones displaying the most rugged crests are built of granite stocks or pillars, which from their hardness, and greater resistance to weather- ing, continue to stand above the surrounding sedimentary rocks. Ihe surface features in general, are those which result from long- continued differential erosion, acting on a generally uplifted and deformed region. Certain modifications have been introduced by I'l »nt IV. •'^-.V r. f ' Vii'M iif Mount "^hrliliiii from SlifMiui l,tik<' ri.AT>: V. MIH 1). 1(1. Vii'W iif vallfj- of the Kiisx River lit Fiilil Lake. / MAiKKN/.n MOrXTAINN, Yl KOX 17 KliM-i il ii'tioii, Hurh RK tlic Kimxitliinii of iii'fiuulitii"* in tlic Unl-WM-k, »nj the Aixmng of th • im in yallty* with drift, thui iubmerffing the lower slope* of the niomitnini4. Tho lakes anil iwnd* of various size which so often oceur in the valleyf, owe their origin, in many cm«, to glacial action. The higher inouiituiii p»aks of thi-t region often exice not txi-eed alKiiit «,000 feet, the vertical lief being from 3,000 to 4,S00 feet. Tho summit of the Christie pass, btitween t'r e heads of the Rost and Gravel rivers, stands nt a considerable clevution, being about 4,525 feet above nea-levcl, but there are roiitrs on the Miumillnn and Stewart river*, leading to the Mackenzie waters, which arc said to traverse valleys lying well below timber line, containing t^mall lake* and on ill-defined water parting at tho divide. Tho mountains in the vicinity of the wafcrshod are not higher than many of the groups situatcil nt considerable distances from it, so that tho divide is not the most important clement in the relief of til ' i-es;ion, and does not form a natural division line separating tlw eastfrn and western lopes as distinct topographic provinces. The devc .j>ment of valleys at the headwaters of streams is furt'..er advanced on the western side of the divide, this advantage being probably due to the greater amount of precipitation, and con- sequently the greater erosive power excri"ise1 \IK VI. ■Ivrniir .,f <;lMiiiil rhy. I!..-. Kn.r. alnnc Shililcn I.;iU.' I'l.MK VII. :i r.4iii p. IN VirH of Itsi MoiiMtaiii* fi'iiiii Km>s l!iv>r. / {I MACKENZIE MOUNTAINS, YUKON* 1» There is a great disparity both in river development and stream grades between the two sides of the divide. On the western slope the water flows from near the divide, for a long distance, through valltys of mature erosion with an easy grade Lefore reaching the master stream, the Yukon; while the streams on the eastern slope fall rapidly for a comparatively short dis- tance and reach a much lower level at their junction with the Mackenzie. For example, the Ross and Pelly rivers have a com- bined length of 450 miles, and enter the Yukon at an elevation of about 1,500 feet above sea-level, while the Gravel river, 255 miles long, enters the Mackenzie at a height of about 200 feet above sea- level. Owing to the great difference in precipitation the streams from the west side of the divide carry down to the Yukon more than twice as much water as the streams over an equal area on the eastern side Thus the Gravel river am ts branches do the work on the eastern side of the divide, while the combined efforts of the Hess, :Macmillan, and Ross ■^rs are required to carry the water from the western slope; tl .iravel river being about equal in volume to the Macmillan. The higher mountains of the western slopes are more or less covered with snow during the greater part of the year, and receive a moderately copious rainfall; so that they are the gathering ground of numerous streams. These flow into the forks of the Pelly, Macmillan, and Ross rivers, which have a general southwest direc- tion before joining the main stream. The grr-'cr part of the main drainage ways, therefore, lies transverse to tlie strike of the rocks, and to the trend of the mountains. The main Pelly river, however, flows in a general northwesterly direction, along the strike of the rocks, and in a valley flanked by parallel mounta'n ranges. The time of flooding generally occurs ccrly in June: when the rushing waters of the streams become powerful erosive and scour- ing agents, effectively removing the surfai-e deposits of various kinds which floor the valleys, sometimes to great depths. These deposits, which consist of glacial drift and silts, form the banks of the streams, but an occasional spur of rock outcrops on the river. In flood-time the water reaches far up the banks, sapping and undermini „ them, and the rivers, with the greatly increased current due to their swollen condition, quickly carry away the material that falls in, so that the rivers are constantly widening the trench in 5419—21 i i _'0 (il.,000 to 10,000 feet in height, has an arid climate, very little wind, and temperature ranging from 80° in Juno to -00° in January. The western slopes of the Mackenzie mountains, of higher eleva- tion and exposed to the prevailing winds, have a comparatively high prccii)itai'on, and periods of high winds, while the eastern slopes being on the lee side receive a small precipitation, and immunity from the high winds. The average monthly temperature, however, does not vary much over the three provinces. June is a perfect summer month with practically no darkness, and on fair days nearly twenty hours of bright sunshine; the temperature sometimes reaches as high as 90°. January is the coldest month of the year, with about five hours' sunshine on unclouded days; the temperature seldom rises above zero, and for several days is down to 60", or lower. Three months of the year, from May 25 until August 25, are practically free from frost in the valley bottoms. July, August, and September are the .months of greatest rainfall, which is scanty over the Yukon plateau, being only LDout 7-5 inches in the year. There are no recorded measurements in the mountains to the eastward, but it is probably not less than thirty inches an- nually. The greatest amount of snow falls during the late autumn and early winter. In March, 1908, the snow was five feet deep in the valley of the Ross river near the divide, but on the Pelly river it would not be more than half that depth at the same time. On the east side of the divide the snowfall is light, being three feet less than on the west side in 1908. Pi.AT« vni. Mi'.i p. •-••-'. iniici;iti-il M.imitMiii- iifiir -oiiiii- "t i;i;im1 Hi MACKENZIE MOUNTAINS, YUKOX sn On and after September 1, fresh snow begins to appear on the mountains, while rain is fpUing in the valleys. The first few falls of snow generally disappear from the valleys, but remain on the mountains, consequently there is a much greater accumulation of ■now there. The small watercourses begin to freeze about the miiibcrrie«, blui>berrici<, red and black curruiitit, and two vurietiui uf cranberry are abundant and of good iiuulity. TIio changv from iiu iirid vliinate to one of greater humidity if ii|)piin'iit by tile ftrowtli. to iiiiy one o«<^ndiiit? llio Pt-Uy river. The lipwcr piirt ol' tliii* river is very iittnu-tivc in apix^aranw, the valley lifiritf boriliTcd by ojii'ii. (frii^^v tcrriici's, mid the inimi'to banks i>f tlic river bearing griivi>H of tall wbiU? spruci". This iiapoet disapprars "11 the IJiw* river, where n riipifed growth of white and black spruce covers the bank!) and the valley bottom, and the slopes are covered with a thick carpet of moss, under a light growth of black upruce, intersiierned with willow and alder swamps. In passing over the divide an arid region is again reached on the lee side of the mountains, where growth is sparse anl the soil is of poor quality. Tree growth extends to within a short distance of the summit of Christie ■, : 3 on the western sid", but on the eastern side trees are not seen until a descent of about 900 feet is niaean are more or lwi>i iiiiiiicrou*, but •re not often met with, except in the month of August, when they tome out along the bankn of the Yukon tributurieii to feed on the vutmon. llluck auil grey timber wolves are ncattercl throughout the n gioti, hut they are very rarely seen during the summer montlm. In winter they nssmililo in paik", and make regular hunting trifw up and down the valley:*, killing large numbera of moose. The salmon come up the Telly river and itn tributaries about the latter end of July, reiieh the spawning grounds in August and are all dead by the end of 'hat month. Thousands of salmoa in all stages of decay were lying along the bars and on the bottom of the Uoss river, when we descended that stream in August. Whitefish, inconnu, and pike are found in greater or less nbund- ance, in all the titreanis and lakes in the region. A net set in any favourable place rarely fails to take some of the above varieties. Grayling were plentiful on the Pelly river, and numbers wore eabily taken with a rod and line, using an artificial fly for bait. (Jraylinf , herring, and a variety of brook trout were the only fish f'jnd in the (iravel river, there b<:ing nn abundance of grayling; but herring and trout vero rarely taken. Great numbers of wild geese breed along the main rivers tribu- tary to the Yukon, the nesting sites and feeding ground being among the willows and on tbe mud bars close to the streams. Scattered pairs of swans frequent the small lakes in the wide valleys during the summer, but they gather in large flocks in the late autumn before taking their departure to the south. The geese and swans do not frequent the Gravel river, ns the conditions there are unsuitable. Fur Trade. Furs are the principal articles of value at present derived from the Pelly river and its tributaries. During the year 1898, and the few following years, numbers of white men ascended these rivers in the search for gold, but never succeeded in finding it in paying qinintitics. Some of these men, attracted by the great extent of country in which fur-bearing animals were found to be numerous, settled tem- porarily in the country to make a living by trapping. •mmm MACKEJIZIF. MOt'JCTAIXH, VlTKO\ 27 Tlic ftw th«t otill kpM av forccl to »p<-ii(! coiiMfkrobli' i.f tliiir tiiiif in truppiiiR nnti«tL'uai'. The following estimate l.y Mr. R. B. Riddell, who trnppo-l f-r several year* on tho Macmillan river, fi\ii^ nil approximiito ially lynx. I* 7,'"io ■JIl.tMII) H.IMK) There were al«o a sniull number of b»niver, wolverine, and Ic.x taken each ycnr, anncrally very icw trc'-s prow higher than about 1,000 feet above the river, owing to the steep slopes of rock and talus of the valley walls. The valley of the Mackenzie river in the neighbourhood of the Gravel river is sparsely wooded with an inferior tree growth. TRANSPORTATION. Small steamers of light draught and sufficient power c;in ascend the Pclly river, during high-water .stages, as far as the mouth of the Koss river, a distance of ^.'.0 miles from the Yukon, or up the MacmiUan river as far as the forks. At least on' steamer comes up to Ross river every siinimcr, carrying trappers and prospectors with their freight; also bringing supplies for a fur-trading pwt at this point. The charge on freight from Dawson is $50 a ton, and for each passenger S.IO; the journey can be made in six days, btit usually takes longer. The traveller who wishes to go further, either tracks his own boat up stream or walks across country. Pack-horses could be used over a limited portion of the country, particularly along the open benches of the main valleys, but the wet mossy floor, the thick growth, and the scarcity of feed in the upper valleys would be found serious obstacles to their use. Dogs are frequently used as pack animals by the trappers and Indians during the summer; a good dog will pack forty or fifty pounds. In winter most of the travelling is done on the rivers, with dogs haidinp the necessary outfits on sleds or toboggan-s. If the loads to be hauled arc heavy, the trail must be broken a day ahead to allow it to freeze hard enough to hold up the dogs. It is quite possible to boat up the Pelly river, but with heavy loads it is a hard task, as the current is strong and steady and there f 30 GEOLOGICAL SURVKV, CAN.VPA are numerous stifiF riffles. Two portages must be mado, cither going up or down stream : one nt Hoole canon of half a mile, and another at Wolf cufion of one and throe-quarter miles, these ciifions being, respectively, 23 and 14.", niilos above Ross river. Two rou.uli bed-rock rapids occur: Hoole rapid, just below the river of that name, and Slate rapid, about sixteen miles above Campbell creeit. A boat witii small load can be lined up both these rapids, on the west bank, and they can be run with safety by competent boatmen coming down stream. Beyond Wolf canon the Felly is navigable for small boats for a distance of at least forty miles. About six miles of swift broken water is encoimtere-ZIE MOUNTAINS, YIKOX 3!) intruded along the bedding plane* of the old^r formation and subse- quently sl.oared and altered. The various rock members which iiinke up this formation have been subjected to such u liiKii deproe of metaniorpliism tiiiit their boundaries and original structure have been destroyed, and a achis- tosity common to them all has been developed. The strike or trend of the rocks is generally northwestward, and they dip at various angles, the strata being broadly folded as a rule. Quartz veins and stringers are numerous in places, but on the Pelly quartz docs not constitute as large a portion of the rock mass as it does in similar rocks at other localities. The crystalline schists have a wide distribution in the Yukon territory, and have been described in a few localities under the name Nasina series; the rocks in the area under consideration probably represent the same scries. Nothing is known of the age of these rocks, except that they are older than adjoining and overlying sedimentary rocks in which fossils of Ordovician age have bwn found, but they may be pre- Cambrian. The contact between the crystalline schists and the Pala;ozoic rock has not been observed at any ixjint where traverses were ma>ires fccn fur the next fifty miles consisted of thinly-bedded «iuartzitiB and nrgillitcs, similar to those on the Pelly river, or of small detached masses of diorite, and andesite. A fairly continuous sectiou, of about fifteen miles in length, seen along the river below Lewes hike, shows n remarkably complex series of closely folded rocks, witli rapid alternation in bedding and com- lx>sition. Thes," consist of red, green and grey slates, or argillites, chert, (luartzite, limestone, saml>tone, grits, and volcanic tuffs. No organic remains of any description were found in this group, but they are placed provisionally as Silurian, for reasons which are given further on. Thr argilhiccou- rocks of the group are varied in colour, and in the degree of alteration, and exhibit a slaty cleavage at right angles to the bedding, or a shnly structure, where the beds are made up either of thinly laminated layers or of wedge-shaped fragments. The most important limestone band in the series varies in thick- ness from 10 to 150 or 200 feet in thickness, in beds of 2 to 12 inches thick, and ()(Miitf ^fc*- ConBlomeratc 2,000 CjarsalUv of thi- (irawl KiMrfn.ni Mt. St-wki. I'lMK XIII. Sikwi Ciiiicin, carvfd in Silurian liiiientiinf. 5U!I— p. :«. MACKENZIE MOUNTAINS, YUKON 39 Of the few of these brought out, Lambe reports the following forms : — Favosiies, sp. Streptelasma, sp. Acervularia gracilig, Billings. Also two specimens of a StromatoperoiJ, Aclinodictrjon Keelei,^ des- cribed as a new species by Dr. Parks, and a TPentamerus, which was kindly examined by Dr. Charles Schuchert. of Yale University. New Haven, who pronounces it to be apparently an undcscribcd species, and nearest to Papillosus. Devonian. The sandstones classed as upper Ordovician extend down the Gravel river nearly to Inlin brook, and are then replaced by lime- stones, more or less maasive, but the contact with them was not seen. The limestone beds are broken into several faulted blocks, dipping to the southwest, with low escarpments facing the northeast, and here constitute the eastern foothills of the Mackenzie mountains. No fossils were found in the limestones of the foothills, but they are probably lower Devonian. As the foothills decrease in altitude going eastward, the limestones become less tilted and broken, the bedding is thinner and several shaly layers appear. Brachiopods are abundant in some of these beds, particularly Atrypa reticularis (L.) and Alrypa spinosa. Hall, and the following corals which were deter- mined by Lambe : — Streptelasma rectttm. Hall. Phillipsastraa vemeiiili, Milne-Edwards and Haime. Uederella canadensis, Nicholson. MF.SOZOIC STRATA. Fossils of Triassic age were found by the writer in some impure limestones, in the upper Stewart River region in 1905, and a large area of rocks was coloured as Triassic on a map of that region published a few years ago. Since then there has been reason to believe that these rocks are Pala;ozoic, and that only a small remnant of Triassic rocks was enfolded with them. A similar case occurs on the Pelly river below the Ross river, where a small undefined area of rocks was found by Dawson to In 1 W. A. Tarts. ' Silnritru StroniRtoperoids.' 40 OEOLOOICAL 8UBVET, CAKADA m ^ contain plants of upper Cretaceous age, but the different character of these rocks to the surrounding crystalline schists renders them conspicuous in this locality. A few exposures of soft sandstone and conglomerate were found lying unconforniably on the chert beds on the Ross river above Sheldon lake. No satisfactory examination of these could be made at the time, on account of the snow, but they are probably of Mesozoic age. About twenty-five miles from the Mackenzie some soft sandstones and conglomerates are exposed for a few miles, along the north bank of the Gravel river; the beds are inclined slightly toward the west, and have a thickness of about 200 feet. The sandstones are coarse grained and nodular, of yellowish or grey colour, grading into fine conglomerates, which are made up chiefly of black cherty argillite fragments. No fossib were foimd in these rocks, and although no exposures were seen below this point, they are probably part of the same series found on the Mackenzie river, in this neighbourhood, which McConnell refers to the upper Cretaceous. The Cretaceous beds occupy the depression between the base of the Mackenzie and the Franklin ranges, and have a width of about twenty miles in the vicinity of the Gravel river. They overlie Devonian limestones and shales. TEBTIARY STRATA. The Tertiary rocks which occupy a basin of limited extent on the Mackenzie river at the mouth of Bear river, are described in detail by McConnelU in his report. Basalt occurs in low bluffs, for a distance of about fifteen miles tlong the Pelly river near Hoole river. It is pre-glacial, and Dawson has classed it provisionally as miocene from analogy with similar deposits in British Columbia. Nothing further was learned of its age or origin by the writer. IGNEOUS ROCKS. The unaltered igneous rocks appear in this region only as small isolated masses among the sedimentary or metamorphic rocks. Granite was seen about ten miles up the Ross river, where it forms a ridge about 1,800 feet hign on the north side of the river. 1 H, n, MrConnell. Ann. Rep. Gtool. and Nat. Hist. Survey of Canada, Vol. IV.. ltj.S8-8», Part 1), pp. 95-100. MACKENZIE MOUNTAINS, YUKON 41 The rock is a fine-grained, brownish coloured, biotite granite, and is intrusive in the crystalline schists which are seen exposed around the base of the ridge. This granite is different to the bodies which sometimes form the centre of the mountains in the sedimentary rocks, being finer grained and of a more acid type. It has been exposed to erosive influences for a long period, and the profile of the ridge is similar to adjacent ones composed wholly of sedimentary rocks. Several important bodies of igneous rocks occur as stocks, or cores, in the higher mountains, or mountain groups. Mount Sheldon, overlooking the lake of that nar a the Ross river, is so formed. The rock here is a granite porphyry, ^ 7 coarse grain, in the form of a pillar, which has eaten its way up through the Palaeozoic sediments. The contact is well defined; the granite has merely baked, and rendered brittle the argillites enclosing it. The granite is well jointed, and weathers into a serrated crest, the argillites being worn away for a distance of several hundred feet below the summit. As the granite stocks or pillars become unroofed they offer greater resistance to weathering than the mountains composed entirely of sedimentary rocks, hence the mountains possessing granite centres persist longer at high elevations, and are also more conspicuous by reason of their bolder outlines and more rugged crests. Itsi mountain and Mount Wilson are of this character, and several mountains on the Macmillan and Sttwart rivers, which are prominent topographic features, were found to be built of granite. On the banks of the Ross river between Big Timber creek and the first rapid, are a few isolated exposures of granodiorite and rhyolite, both bedded and massive, but the relation of these bodies to the sedimentary rocks and to each other was not seen. On Pelly river below Slate rapid are a few outcrops of diabase, intrusive in slates and quartzites. This rock is fine grained and much altered, is traversed by veinlets of quartz and calcite, and becomes slightly schistose at the margins. Large boulders and blocks of similar rock were seen on the lower part of the Ross river, but were not found in place in that locality. Igneous rocks appear to be almost absent on the Gravel river, the 42 OEOLOOICAL BDKVET, OAWADA Sill only occurrence observed being a sill of diabase intruded between beds of horizontal sandstone. The diabase was first seen below the mouth of Twitya river, where it forms a cliil 100 feet high, about 3,000 feet above the river, on the mountain on both sides of the valley. Some miles farther on a fault brings the diabase down to the level of the river. It is coarse grained, and much decomposed, with a roughly columnar structure. Superficial Deposits. The valley floors of the Pelly river and its tributaries are all covered wi-h drift deposits of varying thickness. Most of this material appears to have been laid down by the complex action inci- dent on the occupation of the region by glaciers. A complete section of the drift shows rolled gravels at the bottom, then boulder clay, above which are sands and gravels, usually strati- fied, with silt on top. The deposits are very irregular, and their sequence varies in every section examined, it being frequently found that two layers of boulder clay are scparate'« 7;"^;^^^ Granite boulders of large size are very numerous; these litter the beds of the side streams, and are scattered over the valley slopes. 'bout 'ate S- 44 GKOLOOICAL 8UKVKV, CANADA *kv \n important terrace of gravel about 200 feet high occupies the triangular space of a few miles in extent at the junction of the Katla with the Gravel river. The terrace is composed of river gravels, with boulders and pebbles of sandstone, dolomite, limestone, and slate, but only a few small grnnite pebbles arc present, and below this point granite is altogether absent from the river wash. Where the bonks of the stream are not f solid rock, they are generally composed of the above material, but mostly in low banks from 10 to 20 feet in height. At several points, the river banks are the truncated alluvial cones brought down by the side streams, and these generally con- tain a large proportion of angular or only partly rounded fragments of rock. Sections of a thin sheet of boulder clay are seen at intervals. This material is generally stratified, and contains a layer of gravel and sand without admixture of clay. Above the moutl. of Nainlin broo'', the river bank is composed of about 120 foet of dark blue clay, quite structureless, and containing a few pebbles, the larger of which have flattened and scratched surfaces. Most of the pebbles are small and well rounded, the greater part being of granite and gneiss of various character. Granite pebbles are absent from the gravels for a distance of seventy miles above this point, and they were evidently carried up the valley of the Gravel river by glaciation from the east, the pebbles being typical of the rocks of the great Laurentian area. On the opposite shore below this point are banks of the usual Gravel Kiver boulder clay about 80 feet high, showing bands of gravel and silt. The boulder clays from the two sources show marked differences in colour, composition and structure. Below this point the granite pebbles in the wash increase iu size and number, but are not found up the side streams above a level of about 200 feet higher than the main river. The thickest deposit of drift on the river occurs about eight miles below the mouth of Inlin brook, where the river turns eastward through the foothills. The base of this section shows typical boulder clay, above which are bedded silts, and above the silte is another deposit of boulder clay ; on top is a bed of earthy non-coherent clay containing only a I'HIK \IV. MiMiutuiii-' "t th" Sii.Miiii-i r;iiii.''\ NMtlii I! I'l ATK NV, MACKENZIE MOCKTAIN9, YCKOW few pebble.. All these m.teri.U .re of a dark-Btey muddy colour, and have a total thickness of ab. .t 600 feet. , , . . w .„ The broken plain bordering the Mackerzie is underlain by blue clay with a more or leas gravelly admixture, on top of wh.ch « yelLish sand or sandy gravel. The gravels contam -^ !-«« P-^- tion of black chert or slate pebbles derived from the underlying Cretaceous conglomerate. . _ , . _:„^ About four miles from the Mackenzie the Gravel r.ver swmgs against a clay bank about 200 feet in height, and of a dark-gr^ cLr. The lower part of this clay is stratified, and appears to be quite devoid of pebbles, but the upper 50 feet or so contam scattered ""Te river is undermining this bank, and at intervals large masses of day. becoming detached from the face, fall with a roanng no.se into the swift water. Glaciation. It would appear that during the glacial epoch a thick Kon.nWw.in.. Rh„k.. "U.ve m-mth of Twit.VH Riv.r. VVII. Cliffs of OrdovicUn S«nd»tone, overlying M19-p. «i , .m of diabwe, ^lope. of Moui.t Eduni, «r»»el River. m 'G3 MACKKSZIE MOCWTAIHS, Yt'KOM ZOOHOXIC GZOLOOY. 47 Pro.p.c,in« for ,M began on the Felly n.er m «rly - 1««2j For .o«e v.ar- .uUcqucntly. . few miner, working ou the ,r.v.l ba« n...h. a. n,uc.h a. $10 to $20 a d.jr < «ch. the.r opcrat.ou. b ng craned to the lower portion of the river. Since then pro.pect,ng h«.ten earricl on along the ^.ter part of the river ami m.ny of U. tHhlric-; but no n.ini.,. .f in-portance ha. yet been done n. '^"fT";..! coarse colour- of g-ld are found in the Krav.U over . larr- area. H,t no coarse gold in paying ..uant.tK.. lm» yet been ''^'^:^'\o be a clo. con.,..x.o t,», Yukon territory betiinthe'^Ulline-hi.^ l.ccr depc^it.. In the v. ley of the Felly. the,e rock, appear ' . occupy «»*>».-'-":«, ^;* dUtance ..-about t.n miles on each side of the r.ver. w nch flow, g neTally parallel to their strike. In the vi.inity o^^.^-P^" 'j-^; however! the Felly river turn, northeastward, wh.le the belt of c^BtaUine .-hi^ts continues in a southeasterly direction .long the Frances ana upper I.iard rivers. ,,„,,. ,, In 187:.. some pros,«ctors from the Cassiar gold-field., .n search of new ground., reached the headwaters of Frances "-''«;'» ^'^^ on some bars, obtaining gold which pa.d at the 'ate of $8 o $0 a day. and there i. no doubt tUa. the Yukon gold-fields -uld have Zn en.end and discovered at that time from t ns quarter .f the route ^vc.re an easier one, and not so remote fro„. any base of ""tlr'the last few years work in the Felly district has been con- fined to the streams entering the Felly from the south, from and iucludinK Lapie river to Hoole river. These streaxns head in the Felly mountains, a high -nge. lymg south of and parallel to the course of the Folly. Along the base of he e mountains lies a wide abandoned river valley, floored w.th wash gravels and containing several small lakes. This old vdley .s se^aj- ated from the Felly river by a narrow belt of low rocky W^-s. th o„gh which the streams have cut channels. The gravels of the old valley Tarry coarse and fine «.iours of gold, and the streams m flowing .cr„ss it conccutrnte a portion of this gold on bed-rock. The best prospects so far have been found on some of the small tributaries of Hoole river. 48 OKOI.(M!KAl, SURVEY, CANADA The Duncan mining district, to the north of the Telly, resembles the country in the vicinity of the latter in many respects. Coarse gold in paying quantities was found in that region about ten years ago, and almost every year since then discoveries of more or less importance have been made. In spite of the large area over which gold has been found in the Duncan country, there are serious diffi- culties hard to overcome, which prevent it from becoming a success- ful niininK camp. These are: underground water, large boulders, and lack of adequate transportation to ensure a supply of provisions for miners. Fine gold is found in the gravels all along the Felly, from the Yukon to Campbell creek, but none is found above this point. Mr. Henderson tested a few bars above Iloole cafioii, using two sluice-boxes, about 12 feet long, and collected several pounds of the lieavy dark sand which accompanied the gold. A greyish-white, malleable mineral in small scales, which was presumed to be plat- inum, is abundant in this sanil. The samples were 8ubmitteo OEOLOOICAL SUKVKV, CAM ADA Stream flowing into the Macmilirn river, and that he found no coarse gold at all. The explanation of Wilson's pc.sistence in remaining in an apparently barren field is that l.e i : in s enrch of the legendary McHenry mine, a phenomenally ri"'a deposit of placer gold suppo«°d to exist in this vicinity. McIIenry \i said to Lave been a miner from the Dease Lake diggings, who penetrated to this region on a prospect- ing trip many years ago, and took out forty pouaJs in weight of coarse gold and nuggets. Various reasons were given for not return- ing again to his Eldorado, but he gave certain approximate direc- tions by which it might bo located, and many prospectors have been beguiled into the quest. A great deal of the country between the Macmillan and the headwaters of the Nahanni has been traversed in search of this lost mine. Quantities of drift lignite are found along the lower part of Campbell creek, but the seams from which it was derived were not found. There is probably a small Cretaceous area lying on the schists in this neighbourhood similar to the one at Five Fingers on the Yukon river. Drift lignite is alS' foui.d on the lower part of the Gravel river, which is no doubt derived from the Tertiary coal-bearing areas of the Mackenzie basin. Hematite occurs on the Gravel river about ten miles below the mouth of Natla river. This iron ore is coarsely laminated with red siliceous slate, having a thickness of from 50 to 100 feet, and is interbedded between conglomerate and dolomite. An assay of an average sample of tLij ore was made at the assay office of the Mines Branch, and gave only 25 per cent of iron. INM)RX. ^ Vmrn. 15 Agricultural land •• •• 35 37, 38 Ami. Dr., brachiopods. etc., earned hy • • • j, Arctic Red river B Bacotyeh river. (See Gravel river) • ■■ ^ Basalt on Pelly river ,.....!!! .^ 36 Bow River group " ..36,39 Brachiopods U Braine, Frank Ca„,pbell, Bobt.. Brst exploration of tiard ami Pelly river- by. . ■ J" Camsell, C. re pebbles and boulders on Mt. On«le„onRh ^^ survey of Wind and Peel rivers b> ^^ Cnrcnjou river 36,37 Cnstlo Mountain group 3- Cephalopod 13 Chandindu river • - Christie, J. M., acconii>:»n"l «" ''"■•^^•^ ^ '.'..'.'... 18 Clarke, Mt .. •■ 22 Climate S . 10 Dawson, Dr. O. M.. journey of.. ■ • jj ,. << suggestion by re mountains Drainage system of district.. Drift. (See Superficial Deposits) ^ Duncan mining district, gold in r 34 liaise cafion, rocks of 24 I'auua of the district ^g Ferro-nickel found on Pelly ri»er ,'.'.'..'.'. 28 Fish .... 28 Forests '" n Fort Norman ' " " " " ..32,38,37,38,39 Fossils 47 Frances river, gold on '' jg Franklin range " '' 34 Fruit .. 11.12 Fur hunting " ' gg •• trade .51 52 OKOLOOICAL SIIRVKV, CANADA 1*1 ft Qaroe animala a Geology, economic 47 Oeology. general, of thp district SI Olaciation 4S Glenlyon mountains 15,16 Gold mining 28,32,47,48,49 Ooodenongh, Mt 46 Granite. ('•« igneoaa Bocka) Graptolites 38 Gravel river 11,13.19,20,30,35 " " district nnattractivr to prospectors 49 " high clay bank on 45 " origin of name 11 " rocks on 40 " source 8 " survey of 9 H Hematitp on Gravel rii-er 50 Henderson, Fobt., services of acknowledRed 7 " tests of Polly River santl »8 Hess river 1!) Historical spmmary 10 Hoole rapid 30 I Igneons rocks 4] Indians II, 12 Iron. {See Hematite.) Itsi monntain 41 J John lake 30 Johnston, R. A. A ^j, X KaUas mountains j5 Klondike goldflelds, disoovery of ^ '''•'• v. V. 13 I. Lambe, L. M., on fossil corals, etc 37 39 Lewis & Field, traders ' U Lignite found on Campbell creek and Gravel river 50 Limestones 84,35,36.88.39 IMDVX. <• snrTcy by MrHenry mine ■■.■. .. .. Mackenzie monntMnsdefinea.... • •• •• topograpny of Mncmillan mountain' .....!.• ■• river " mirvpy of Moce^kin boat, n^ by Indian" •• Mountain Men of Gravel "'"" " "^ w. . .. Murray. A. H.. Gravel nver mentioned By Nahanni river Nnitina ««ries ."'i/nnV Navigation. {See TransportaUon.) 53 Pao»! ^^ f Pelly. Sir H.. river named ffter.. .. .• •• •• Pentamorus Pettitot, Pftre •« " map Pike, Warbnrton. ionrncy of ■..■*..'".", Plateau ranges.. .. ■• • Pr«vo8t canon, rocks ol.. IS . . . . IS. 16 .13. 15, 19. 30 48 ... 9 10 IC 89 18 It " . .. 10 IS S4 ied on survey by. oAA^n R B.. acroinpaniea on »u."=.t -- Riddell. R. B- t,, by. of fur values K.'S^^l^d.^blef factor H^b; Co., rWerna^edafter. ^ ''Tr-d^tri;; unaitracti'veto" prospector... •• •. ■• orisin of name /'■ 'J ' .. . .. .. rouu to «""""" "' •"°"°*';'°;;- .;• ;; ;; .. . <• •' survey of 2" IS . .. ■• W 19,30.35.43 *9 ... w 8 9 W oKot.ooirAr, mukvkv, canaiia a BandstoDM ^*^ Sa7un*i range ,, Ss-yanne-kwe mountains j^ Schnchert, Dr., brachiopods, etc., namrd by as as Sekwi. Mt ' " Selwyn range 'u Sheldon lake 3q Sheldon. Mt .................. 41 Shesal oafion w Slate rapid 30 33 Stewart river ' " ' " " \ '13 " " explored n Stratified rocka .' " 3^ Stromatoperoid 39 Saparflcial deposits 42 T Tigonankweine range 14 37 Ti-konan-kkirene mountains ' j4 Timber 15 24 28 Topography of the district '. .' ' [o Transportation 29 30 Twitya river. <5ee Qravel rivir) 'u ▼ Volcano, reported g W Wilson, Charles, prospector on Ross river 49 Wilson lake 39 " monntain 4j Wolf caiion portage 39 " rocka of 34 Y Yukon plateau I3 n jg " route to via Gravel river 11 CA5JADA r,rrxivKT OF MINES 4 H. U)W, Utrctt «!««•"• > Wn^D LKt OF luxmiTS and mai>^ „, ....xnAi. «:oNoMic >NTKU..:si ^1IKI> lllf Tilt" H 111.1X11 .OKOl-OCaCALBtUVKY, Report, of the Mi«- •••«;»;:,, :,., ,^,.,. Kr,.on o. Min-^ Sci'iicn No -MV ;lol I. '.••'■ li,.,,„rt o( Mi..o»^Se.-.i"n ls'U-4. 71 » SKI h;i:> SfCt 071 1«'<7. IVI*!. I'.V'l. |^> Ihs. ISHS. lh^O. IKilO. is«l . lSKO-91. 1S77 f.l2 f.2:» 640 071 6SG YearlSOS. 1S04. ISO.'.. 1M»'.. lS.sf.-96. 1«>7. IS'.IH. Ih'jO. No.7t9. Y-.r.;;oo, 71'.>ii sj:« Htil S'.Mi 024 9S1 Jlill. I'll 12. >'.»>i;i. 190."). lUOrt. «»;.«.! K...»-. B-^.«- No. 'SIS M.-.l. •S.''>4 s.")7 f>5'.l I'lnt immi fiml ln(ii-.'ri;>l Earth Mnnpinc^o. No. «■•"• Jip""- a?':VMulyb.lonumand ° ■ TunRsUn. 877. Graplii'-e. HSO. Teal. So R.M. ri.o~!'l'»<" S.H2. C'M'I"''", ,,. ,„„,, (Ircnii'J. f.5'.l. t^uH. 4 JClneraloKT Year 1874-5. 1875-6. 1H76-7. 1877-«. 1878-9. 1879-80. 1881V1-2 ^ « 18H.H-9. ^ . 1890-1. 3W " >^«-!-3- 580. Year V^- 111 - is;««- 794 i8^»y. Li\ ' 1900. ^58 " 1906. -— - ■ marked thu. .re out ol prmt. REPORT& T4» •07J •20() 205. 687. •WW. 043. 051 070. W>2. 1016 lOAO. 313. •23-.. 236. 263. •271. •294. •.'.73. 574. 743. 039 040 9.S0, 088. 906. 1035. oy.sr.RAL. Altltiwlr* of raim.l:,. by J Wl.iif, iHim '"'VminK' '""''"*'"■ "' *""""'" •"'* "'-■'"■ '>y «• A A. Jolm-lo., „n.l O \. YUKON. ^'"^"^:^':::ir ''y *' " i>»««..ii. iss?. m«,« n.«. 274, nc„u- m m _ i in ■ -■•'—-<■, ■. Illi- S 111. — 1 111. " ' ■k iik.jn MI..I Ma. k. n/1.. I,n.ln-. by H O MH'„nn..||. ISHO. M,i,. \„. ri(,i. „.„!, '^'""►'illr '",',',' '"Vi '''"•"""■""■>•'• '-y ^ *i M.Conn,ll. HMMI. .\|„,, .\., ,iss, Kl..n.likt.Knhlfi..l.l, i,vU.(i. MKonnrll, lOfll. Map .V, 77.' .,al.-.|„ _ 1 in UpiHT Hiinurt riv.T, by J. Kwli-. M.ip No. 038 1 wrjili' .H 111. M- I ill * i I» . . 1 . .1 Peel mi.l Win.l river-, bv Cho.. Cmu-.ll. Map Vo ' '"*""r. '•■t.!, HCMie >» III. ■- 1 in. Kl' "• "• «'^'i™'- 'ooi .m',."no. '"°"liiM,V"aTe%r'i.'l"l ir""' '"' ^ ° MoCmmll. (Fremli). M„p No. WliiNlmiNc f,.p,«r IJelt, by H. O. MrConnell. Map, No.. I,(i2fi, 1,011, |,,)M. BRITISH COLl'MHI.X. The Rorky mountBiM (between latitude, 40° anil .•.(•. 10°^ bv O M n.«. „„ 1W6. Map .Vo, '..aa H, ale 6 ni. - 1 In. Mu" No 224, .,„fo li m ~^^T No ii?'""".!" "■* «™''5K'.'-»' -""-"TC, by /{. <;. MiCV.nnell. W \Up •337. S24. Van 111^ ••>"■■• (•■u.iiii ti u... K*'uiu||[ii'ai •No. 24H, f-rali- .i III. — 1 in. Carlhosi Mmeriil weallli, bv --l. ^""'..'^."'I'in"' '^'■"■''■'' ^y *' •^'- I'awon. 18.88-0. Man No. .m, .~,nlc S Knniloops,listri,.t,byG.M. Dnw-on. I,>.l-ri..|,l, of' M«nitob«; HMk", "'ule 3 m. - I in t; R •y.r:!;^' 'S:^^^':^;,^;::;;;^.^'- ""ti-h c.u„.,>^ 213 KfiM fypr#«< hilN iin.l W, 8A8KA mil;W.%N, 204. 32.^. 704. 70.'i. KCtS .>.•« ■ ""'' **'"^1 """II ^..1 aoil ai'tt. male H m -I m """• ""P" •■«o»- MA.Vi iOBA. N!::;i^i::';„^i:..,''{;;^. "j-'r^ry^.:^"" >"- ^i*. 3.«, 3.,. «'»I.Mn. -Iln '>frcu iwiit-i. M«|« .\,„ 339 »n. J 350 217. 238. 239. 244. NORTH WKST TKimiTOIUES 207 S78 •«84 618 CB7 6«0, Att.wapl.kat ami .VIbany riv.-V. lyU n,.|i i>.>m> ilAfn^a Kbit nn.l . _ . . 7)-fi 815 Sin 905. .^-" .nap .-NO. :»5, , _ -rale H ....HTln "" '^'"' ^^' ^' " "°*''''R If'W. Map No. a7«. ■ '•auraclorpfnin^ula. bvA P Lon. ifcor \t -.al,. J5 ,„. «1 in. •'^^" ""'^' '->• •> "• fyrrell. lM«i .Map No. COS ^""Map'r ^!;y'ri:'^v' rV"-- '-•>•■ »'^ « '«■.■ 1 ' "" •"^"""• .. Hni.-lin. .»•». 1.1.0W IWK). Maps . N.w 779. 7H0,7S1,. rata OXTAUIO. 215. I.akcof ihc\Voo4, uv ., ,1. I, Bniiiii. iv.iim. Map No. 342. »en n 4 m - I i iJ. V.turalOjusandt'etroleun. bvH.P, H. Ilrunull. 1N()0-1. M»p.H Xo. .Tl A -■ <.".? "u- 'eterboroUKh, and flHstinK^* .ounties. bv K. D. A.lain,. IMtJ-:) '■ <'nthel'r,.nre.,bvlMl.ll. IsiW. Map No. 570, male 4 „. i 723. 739. 741. 7'JII. IHil. Q(i2. ISOO-l. Map No 343, scale 4 m. -1 In IVio-l. Map .\o. 342. iicnlo 4 m. - I in. l-:t»u. Stine river and l.alte Sliebandow.m i.mp-»l,'cet«,'by W. Mclnics. 1897. Map- Nos. SSi) and 5(i(), male 4 in, -1 in °°ijiT"''» "'"J'' "'* Kingston and Pembrol«- railway, bv E. I) Incdl i uc'bcc T" "^ 1 '■"s'-o" tountira, by R. W. IJU. 1S9«. (fee No. 73y. Ottartu and vicinity, by 11. W. ElU. 19(J<) 1 irll. »li,-,.t, by U. W. ElU. li».)0. M,.p No. 7K9, «it^ by A. E. Harlow (Hc|.rint1 < '.•'• *'-"'■, ■■;;:'.''"'. ', "> - 1 in. ; 824, s2.5, ,sti4, s, ale 400 ft « 1 in Alpis>ing ami liiniskaininK map-sli.et.s, by A. E. Harlow. (Itcprint) .So.H. oWl (KM,, scale 4 m.-I in.; .No. 044, s. ale 1 m. - 1 in Sudlmry .Nii kcl anil Copper d Mapn Nos. Map^ 998. 1075. . - -"1 in. Repo^rtjin IVmbroke sheet, by H. W. Ells. (French). Map No. WiO, scale Gowganda Mining Division, by W. H. c„l|i„s. Map No. 1,076, scale 1 in. ~ 1 in. 2ir,. 240. 2ftS. ^7. 328. 679. 691. 670. 707. 739. 788. 8«a. 923. 9V2. 974. 976. !I98. 1028. 1032. -1 in. Ells. QUEBEC. Mistas.sini cxiK-dilion, by A. P. Low. ISS 1-3. M.ip No. 228, scale 8 m tompton, hlmi.teml, Heauce, Hi, hmond. and Wdl'c ,,„mtie. bv H \V Mcganlic \'f''';:;'-./>o^'^r''''.,'-^-i:. H.;ll.:.l.a.l.crt, by It. W. Ells and F. 1). Adams. 1S94 .M.ip .>o. .xl, .scale -I ti.. -= I in Laurent ian area north of the Island of Montreal, bv F. I). .Vdaiiis. 1,S9,', Ma,, .No. aW), siale 4 in— 1 in " ' Auri^-rous deposits, southeastern portion R. Chalmers. 1895. Map No. Eastern Townships, Three Rivers sheet, bv H. W Ells ixos ArRemeuih ()ttawa, and Ponti.ic counties, by R. W. Ells, l.syj. ' (See No. 739, Noltaw.iv basin, bv R. IVll. 1900. (Map No. 702. s.ale 10 m -1 in \Se Is on l.hmd .,1 Montreal, by F. IJ. Adams. ' jOl.' .Ma,,s nJs.-874 ,"75 S7U ( lubouKamau nuii.n. bv A. P. Low 1905 "■ . ;;!;"■•;, t7 ■'' /•-. Ranow.; fRepHnt). Maps no,. 599, r.o«, Mail ■» m. =■ 1 in , 9H, scale I ni.-l i.-. Report on (•opper-l.earinR rocks of Ea.,tern Town.sl.ips, by J. A. Dres-ser. Map .No. t»(h, scale .8 in. -- 1 in. ' '''"'i'-rJnllo"'''*'"'*''""'^ ■■"'■ks of ICastern Townships, by J. A. Dr.^sser. Report .m the Pembroke sheet, by R. W, Ells (Fren.h) Report on a Recent Discovery of Cold near Lake McRantic l>rcs.ser. Map No. 102!). scale 2 in. = l in Rei-ort on a Recent l)isc,.%,.ry of Gold near Lake McRuntic, Dresser. (French). Map No. 1029, scale 2 in -1 in , Que., by J. .\. Que,, by J, A. NEW BRUNSWICK. 218. Western .New Brunswick and Eastern Nova Scot la, by R.W ElU 1S,S,-, M'ln No, 2W, scale 4 iii, — l in, ■ ■ -i ai9. Carleton and \ ictoria counties, by L. W.Uailey. ISiSo. Map No 231 seals 4 ni, - 1 in. ' ■ 242 2G!). 3.10. 661. 7!)B. HiU. 9,s:<. lU.'i4. 243. 331. 35». 62H, fiS.5. 7!I7. S71. Mineral re.-.our, ch,' b/it \V l- li"^' n"r"'' t^"' ??»• "•»'" '« "' -r'n y«. V. Ul.. (Irtn.!,). Map No. UUU. scale 10 m. -lin. NOVA SCOTIV 8ou,..w...e™ Xov.S.o.ia: by ... W. „„ney. 1H96. tambnan ro. ks of tail HrnV''", ""'"^ '^■"^ "SZ. fiM f.54 o. Map \o. on. sruli- S ■wie 1 ni. ^ 1 in. MAPS 1042. Dominion of Canada. .MinoraU. Seal, 80,5. 891. S94. CIO. 990. O'tl. lull. io;w. inn 1UL>0. e 100 m.-l In. YUKO.V f onra,l an.l Whi-.-L.", •;,„„',■'' *■''"'"«■■ -il Map, s, .nic 2 m lantahi., ami l-iv,' I ,m. l""""? J'.-t"' ts, scale 2 ni- 1 „ -1 in. 278, 604. 771. 767. 791. 792. 82,S. 890. 041. 987. 0S9. 097. 1001. 1002. 1003. 1004. 1068. 1074. BRITISH CX)Li;MaiA. Cariboo Mining di^tri.t, scale 2 m _i ■„ Special Mapof ir,"si;nd T '" *"" "i^ •''■^•'-'■"'. '^ "l" 4 m - 1 in Special .Ma , of iCJCj f."l"'Kraphi,al .h,^, . ,S u|o .,«o H li i„ I ossland .^^il.inK ,-a .m npr"''*"." "'"■♦• S<^»"'- 400 ft i I Fn Uossland .MininK c,^ f' r? 'i *™l!'''''al "iM'.t. Scale! "ooff i i sh«.p Creek M"^i'n""'imp°"G:s;;fJr''ri- *■"'•' ' 2^)0 fr."!iiV '"• .1 In. 1 in. 6 ALBKRTA. 594-696. Pearc and Alhabanka rivers. ccbIp in m. -1 la 808. Blalrmore-Frank roal-fieldn, gralf 1K(I ili —1 in 892. Costiean roal La.sm, male 40 rh " 1 in 92i»-93fi. ( a.srade coal ba«in. Siale 1 in. =1 in .SV^'^'iJ'.L *'°"'"? *!""","''" ""B*™ f"'l Anas. Srale 2 m - 1 in 1010. Alberta, Sa«kat< liowan, and Maui ...i.a. Coal .\rea». 8<-alc 35 m -1 In. SASKATCHEWAN. 1010. Albert*. Saskatchewan, and Manitobn Coal Arca«. S 9H.> 1012 1010. loan. lO'tti. 10:t7. llMli. NOVA SC,-II.\. Prpliiiiinarv Map of SprinRliill coiil-fi.l.l. srali- 511 rh ^ i i« I'iciow riinl-ficlil. siale 2.") .li.-l in. Priliii'iiiarv (JfoloKi' al I'lan of NiciaMx un.l I . .rl)r.j<>k Ir.m ,li«rli't »r-i!i- ■'.-, ,!i. nrniriil Map of Provini c .^liowinn Kold di-.tri.-ts. .siak- 12 ni - 1 in l.i'ip igai< Gold distriit. srnlp .'viM) ft. - 1 ,n lliirri^an i iiild disirirt, .-^-alc -KHI ft. — 1 in MalnEa liiild district, srale 2-">(( It -1 in. Hrooktii-lil (i.ild disiriit, si-iili- L'.")!) ft. - 1 in llalifiit (;i-..|..ci.al sheet. No. »iN. !>. nli- I Wavirlpy pt. No. 'i7. S..-ili- St. Margnrct Hnv ("ipoloKical «.lii-ii Nii 71 Wind-or (ii..l.,tti.al siicft. No. 73. Srali- I = 1 in. tn. ' 1 in. .Soal«" 1 m. — 1 in. I in : ».■ -i.^-r,. .1... I.). .-»(-;iii- 1 n: =1 in .\spotoRan <;.., logical sheet. No. 7(1 .Scale 1 in. - 1 in Nori:.— In.lividual Maps or Reports will be furnished free to /«;;m tldr fun . li-in applifants. ' Hcivirts and Maps may b« ordered by the numhers prefi\.'.l -o titles .\|-.|.ii<;ations -liniild be addrea«ed to The Director, i icoltigi. al Survey, meut ot Mines, Ottawa ey, Umiuri- ■ — S^i' MMMCOrr MWUITION nST CHART (ANSI and ISO TEST CHART No. 2) m ■2A |M lis . ■m itt L£ ■ 2.2 i^Ui ■■■ SI US 12.0 u III^H Sus 1 11.8 1.4 m it 1.6 ^ ^IPPLIED IIVMGE Inc SSSr. 1653 East Uain SIrMt RochMt«f. Nt* Yortt U609 USA (716) *82 - 0300 - Phoftt (716) 2M- 5989 -Fox EXPLORATIONS \m„ fSni- :i£d !!~- :tV«|t*aHC 'M':'"* iV ■: •^ ieg. wmmmmm Hrpartnirnl nf miiifs GEOLOGICAL UHVEY Hon W TtMP.CM.^ M.N,5T. . . j, Dt^ur. M,.ti. VMYa, T 130a I20°«r 12ffb. 12H. IL'K J> H .' MTEDUM 4-^-. >---'' ^: -r J^V- vi:-' t^'*-'' t'?'-" X 5^:^ -7 -^ t>: fM<- ilOO' Ilfs V ) N . STl PI 12H 127* 127'( 126' M- 12a*< NORTH WEST TERRITORIES Ut^^tUff .H,.m ir - ^ — ^-— \> I Bb^- T- ;^ -^~:^^?^^ -^-N'-^^ I ! ;';■?«' M ^>->*^ \ \ \. ^-.X- [Bmi - ^. y''pl}fh ruffffed Mount^i, • A &•;- A --J/J y.-^ 'r i' 0) "^'^l-S^. )mii-' ^^ 1_ yi<^-^n.j!h. !^, 1^1 'wlX^ .> ^ ' \ ' I - - PT' ^J ^ '-^... c T/ A c;- ^ ■'^.'6 >---" atef '^ %y'- v> .y- \t 4--. "'»<**•«* ^,^^ KE£LE_^ PEAK **^ '■',**••' aior i "f ' \\ "^..^ <> '' \ ■"■••..M/fMvtaftaOMc^rnMr .naua mm* tr<-mm* ftrtnt <»»• Brrimf mmm. Th»p mrm n ^m M n i mm m mrO .r ■■ imitu' W IA>- JtMt*y JTMuatolft j y j w. «•< »a« ■ iwiKiMiiin vMM */ **m< S*« mllM, lli«»»nrt< ml— 10 «** Jfa<-M4ll and Z^nr netnwd far abowt ^170 mu«« nmrli m-ttxHp /^^m UmrH Hmmrmlmtm^tm fmnmfimr rimmr. Thr ••»<>«< iir»»««i» MMM* Mt as mfUIUd, tm/^rwtrt •»« mm* r>-prr««fi«c« ty a n m ^K tti' * rrmmp mf It-r-valBr mmmtm •r'<* muMorSH* yMl*« H«jtf>»- Jn t^rwtt «trmtftmrm •Ml e«lMM- /^m IA«mi to tiUi ar<||«, r*« ir»««ll' i i pxvtoa f a*« am M< aprll »ar* fi-mmt Mo •al<>'« >»» » «a u . ia th^ *astf-rm pm ri i m m the Nt««Hiar Mm r m at m n U mmm l ft M i' ■» fitr /Wk«, (M M«M/WiN Mr Patfy. « "'^-TTfr n oiii.j »*m»mmtf Mam ritmrwUhfsrtmf ml m—Ummd Wmif m. Om M—m H—r, lUirUtm Mk* <* M« NmM a^»MM >r awM •'UMtt fak ■ » ■ > »<. Tlka Srm—I >M|r *« tt tmtn t t * ky »M< Am> AMtaWMft to «k« immC*, pr t t i r u U t ml ktgh iMtor tttf it |« prmtMmttg HKoumr. • !•»«»■.■» tii>» l to *. »»f «<, •MM to t« n i v t m iil lf> M<« arva md 4m mmt a j i y i to rM » »■«»>» /*tHnl Imllir Mill* in* M> .nM*> fmm^aim mf M» J(ar*nu<», dl/fiir* to Many »-»iynto /Vuni Mat to Mo MWMarartf. JTraaMy ttddmd Umtimtmnmm, dmimmuir,. mmmdmtmnmt m»d nmgl mm t rimt m , ataMly tvaaMarlMy tm*rli,kl mmlmHrm, ar* (*« yrMatMN* rat**. CmmihHmm, OnlaaM.ii. •m4 Ji ii iaa l aa /'aa> laara /bM>rf a«a Miitot ur mflmtmUtl" or tus /SutI /.rau /Saaail, OU atoat i nimr r m l int jii n.>|, ia BMWiHraW/a ( W ara rf a —to . twMaaMn* a MMrfia ar rn.fr Oaaakrlaa kariaa*. /•• t»a a a a to »-w xaytoa, I gaaaa a rarAa ■wra /a rtaar, a ««ll << « ataa., ataa« f •• /ha> aMaft nk* atoato mf Ma aaUiiifr 4<|> *ato« toaWi Ma a a na H »«p »a« a> < y Wi t >t, |k, ,,„- n«>-!artlf. Jtaatttoir atari MIMa« »/ ■laaatotaa Ma\ r 'He • 'I - JT .>,\^ r'--i -'■''] ■ '^>N. .1 ■ f' , *'"' 4^ . .;^*v .-Z/W- JtlM .^■-r--:: ^'^ V .' ' ''/^.'-i;-' --^^.-^A J^. "-0; 'J I -■ ^^#'^y -*,- *A '•^'.^ <* 1 ^m ^i >«(.,> Wf,.»« ,tt- ■-',_ 'IWnrt .^S' ■■l)' ^) .t. ~, \\oy'- )V ^k > Jl ., o1 ^)-,-. ^. ■,(t' '^)))'^ \ I I I ^4' ■ «»~_^:i^. C.U.Hrn^iiI.R.A Sr. t^r-^n,^,,. , .r.D.Kirtin, /A«<«i^mmm« V.Vl ^•^ '»*.■/■ /A--M.M**(„„/, \ 'i-.~-< 1. iC*ri' /TV'-. *'A' \ tn \ \ \ \ \ \ \ 12S'a Longitttde yift ISHto fioni (Trrrmnrh ll'H. PELLY,ROSS Axi> G1?AMi:L IUM5 YUKON and NORTH WEST TERRITORIES Scale ; so«.BM 8 MILES TO I INCH Ja nhSihir. HI (ft \ \ \ \ V \ \ Mirk, - fit'*-** .!» thf Mtitft nuH j..rt** « .tt.i,t, h^twfrn '■•**Hfltttfithr Irrtir .irrMM 'I tt.i »l , ^n»u* f*ft*ftnp *^niitt*H *»rtittif tin «»• Hf*tiltr*t, Hmfnwn**tt ur*H ».-•#■ «t ,7"' "• furn*. mtrurtMrr amit minur frtttu Ihnm*- t; th^ *^r»t a/ to. I' c'-tM/, "/fcr trfMl^rn /nrrttttm i>f thr m*.mt»Ht hut *•*».. rmUrn^ h»rif*y -r^f^^. hnrmt „r fnirtlif iri.t../../ mhiftfm «/ n« Ar «it ■ falttm. Th'- r^pinf* Mf/ tr-. * .1/ **-■ \litrt -tttte ntout^tnitts ^mfuriitiiMf If Idtr r^ti^/, tMf MtHm ttnrif^n yrorrftf Wor«a«<<*M 'fmh*¥*tt l.ri»o/>r«afr«m> aM« frcfl #•»• 0/^ H.tMHt /■*•*■* mhnrr IA»- 'rt^tm »/■ rA^ ftrinfiftMl rirrt-m. Th* r^ifinn is rhnrnrf^rit^ti ^'|» 'nwy. ff^ntlff «lwfii>»ir< irr^yntur hlll» rmr^r^ «/ih«»«# r« 'Artr cMmMttJ* iWfA w «AiM yrttfih of m*Hall mprttrf mmtt bMtmmnt tnrf fAr m«jM rJtvr* tend CA'-'f rhirf Iribrntttrif-a orrupy '^f"M^, trvff fi^rrtop^tt tftl/rff*. TA***^ mU^pm hnif fttirig >«••-/ ittHtTB, oftrtt 0^rrr*it ntH^» in tfidtA, mn^ rmtttttin tnm — if tmtmfl Ittk^m tinH pHnHm, ttimm ^jr$^tnnff A«^r^r- iN^««f«rw>a 'tn4 i/rnr^m of g*Hni mprurr. Thim typm n/'roMnfry 9efuj*i^% *t ti^fl ejrt^wtHittff anuiht'mst^rlif f'mmt th* f'^flff nttntmimirui, i*tH 4»tilnt^H, hijfh ffronp\, <« fAf HftrhmMir mauttUiina. Th^ high mmg*'* of ihrir • mstfrrt aitl^ ntmng th* fimr^ rir^r, ur* aMrr»-^^H. ,10 ntil^m irftn th* Mnrkmzif fiwtr. by n hrlt uf fonthUlm mA«mI .t.ttOO •>rt in hfigM nhnr^ a»>a-l^r^. Kasttmrd th* foothUls dfi^in^ 'N h'-ight an*t fintiUft trrmtmmt^ tm m krwItrM, tnw^fnt ptaiwt, '•urfirriHff th*- "•firrMAif fif^f, trith am rirrmtium of tthtut Thr Mvaf^r- ifiapma 0/ thr Mnrkmntir mmmmtnins mrm tftm ■rnlhi-Hng gmntut nf nHm^rnHM mtrrmmm that ftow tn*m tk* I'rttu. Mm^ntiUMH fiMtf «*«•• rir^rm. trittutarir* nftk* S*Mlt«t». 1 »H^4tU pttrti^n •/ IA«» dmim^gt- nf th* trrml^m mtnprm. in th^ •I r*a jA«m>h >MHir thr »»mth*rn h»rti*r *f tkf mmp, falls iMta />«»*■•■* rh^r u^irh Joina it** lAnr*l, a trilputttt-jf nf th* tfnr-kettaim. Th*t dmin^ff* nf th* *nal*rm mtnp*m nj th* »t/m$*9M >« r**rie*4 kfi th* Mnrk*u*ir rivrr. Om th* w*a1*m »l**p*m. >rh*r* thm pr*ripttmiio»* *« li*mrp. thr atrrama nt*nn*lrrr thrangh iritir, tr*U •i^t>*lnp**i mlirfftt hmring *m»p grnwlrs. tn the *i»sl*'m miflf, tfh^rr th* pre4^pitmli»*t i» tight, th^ (Jrainag* ch*nn«jr««*, **'Af nnrtgnt ititt trhm th^ wMt*r < tuk* nr *r*H H W»«»« Ink*, f If If rM*fr »* m mtrrtrt- ••/ ?f/ »t*"ri I'Hft't* pn»t *rA*^A g>-- r%r*r ttitt^ hf ilfsr*ffl*it *y rir#>r mtut4th. prff*mhig at h in$tn*MaltiJ* tn tnk* <» l-nttr't h" Uh «.»/., , tg nnrty4 '•• *hf n.*'Mttt nf ti *!■' tntUnn tu i '■ 'V"y. h»,t,tt >,»■ '•■ '>*'y lf.r ml /»« >' 'h fturinyr nt H» ■■>-'* t'tk* tm fh- I • i-r nut Ih high ■■"•I i„ tfttrh^. J -tfr, „f mwift u-Hl •■'» m f p*»rfngmft, '••■•It rr,t9n fmirhu Ifh trtifmr ttui it t. it up rit'**\ . 1 ■■'-•f iM Ihr y*giu ■• ••r>-ur 'titfg th 't irojtl** r >« *■«»•»» ^ r ■ nr*a rnt4t 'In tt t,ihtf*9t nt% ftnl • itntt rf'tr^nmrm "nfutnr- ■ ■ «rr regnritft mm p**- **rrf»»-(<^ *<• ■ f*tif/ rtrrt aAo.fM (W th* Ji '' Ttfg m**u$ In h* *t,M/t>t**l to I/:. th' ntrth *h*»Hgh fnunt In fh- >' m Htl'- r-rtniH ttllrf-tt iffrtf-- th'- ini-l(€ (I rt >Mnitlttf»t*r-Ht*m, ttm- *t*'Hrm mtfl 'tntutftll* ntt I'/' #*«•!«<«-»«•*«> agr, r»"'li*»g frtnt* I pprr < .HittiH* t»'-**^**tMH. Th* gi ••****■ pnrt <*/ eA*- nr* fmm tkr i'*il»t fntlt-g lv */'-mm# .SrArtr* »m tkr 1 im Nnrff WMtM hif mhtil*a itMil -l^lt**, nrrt*tnfH»9tifd i nt%'l n htghtg tttttumtrd. hf-'tH*^ r9*k t-f/^rr^tt Itrnpfnlit** «/ I ppt'r ttrtl-'if-itim Hg* t^^rr /.*« mhutf xM Itu^m .-irt-r fhwul /irr mit^m k*lmtf J* httntl, m*w^riit n*U*m •riff'. "' *nt*iisttM*^, /tm* gln»M*rntr, ii*»a rtmit^ at%44 li»*wMltn»*. crfmrnra P*ll\ firiMitguf tittttf ranoM »*tt»t. *^*tUH—g in d*t*rt44^**- rrMMca ICmmt Htntm rupiH uu f*Ug r*Kmr. Tk*i rcrka, ui rur%o9tm /tmints, ar* iiUrvul^^ kp •tn* iftnevHm rork: A MMM^rr of hight^ nfmmtnit knniem to A«* rttmt p mmrti »f grnniu mnii tJnmkUtma h^fk iH-nkm mnd m»9mnii»iH grottpa Mt>« th^ir ruggmHn»ma to this rmuar. Th* MtiNitm «/' th*- %r*mt*r„ pcrNMt •/ th» mnuHtaiH* A«i^«t, thtMigk witt^ tnanp tmin9r «f gen*rnl H*rtk**'9»t atrik* nttd ttip nl rarioHS «Mfl th* itBr$4**n^ mr »outktr*at. iu a trk^l*, th^g < fmlH*ti.kHt iu plarna th* jnidiuy ^a ri«ae„ Th^rtt mf fnnlting. mntl th* r^p*titiaa of aimUimr kmt Imng diatnttfttm, th* amnt* inH>„nlimn, wmg W < *«ii^««4 f«l*lm. HI Ci gg um rli UHi IZ7^ 127W 126W 1-h; f RAMilL ST TERRITORIES NCH SOURCES OF INb'ORMATlON <''.M DowBou.Ttf^ K (1 VrCaauell.V W (irtUvif , IftHS. Miit> '■'•tnpilation. hy :- •' Keele,J»«?. Is nrigaht,- hff 9mMtl ftl tttntl» f>r rnunrm If Itntt $>tU mtlr» If HutUm nnH H «*// th • limit n/ h*^t high mimp^rn. Jiihm tl. Ilrlftr I ^trt-m ' uufff. ifith jnMr 'V^. I If iimr^l trhu hrauk t*t lA* t it t» j'rttrfirnlttf N|/ thf f'ifri nf tk^ ft*'-!' '•; iMr tH4tf. • I<* ttttt ll/tfH'tr I" t- itt/'tfMun rtr^r. uirm aif f>rrm>'*»l, thr r*"'km art' rut f wtp nt^ittlff •/* «-«, rM^ttm, aMMp^r t nm^hrimm *• r Mrcft fJHt'mtltmp lAr tirmrH rirrrf ttirtt htf ^m«> > kmiU with, tnH^r I W dmm t* or#r- /*«• V'iov.V "/ **•■ -*i«« tkt*t *** tHw ,rr*tM-ttri1. Hrttfitff hr'hifl limrmttfMfa flntrnmi'- a*itft9tt'Mft 'IK I )*«My/w*Nf*r*«fr«. Hf^tlif trrfilkrrtH0 l« Af*l' r«fitMr'«, wr thf profit Hi f II Kin K t. * 'in**! ItfNt tfrHorir- nur4 /fmfntintt /tut»tls »m-* /ttuft -if .« mmmiAt n; htruHt.- I»l Ihr fim»»< I'lrtHM /nmrntt. tkr mturt iHtrrrmltttg f/rokuhti, »« »f My jt*//.> t ,>inrm»tfnmi»t it.lirfiliHtf n Vi-hil»- "r f /- I nuntrmit fftrttuM. Ih thf rHimtftn '•*if4t*H. lyrtrnut r- iffrr ftiMnti nntgat «»»*#■ Iftratilif trhi'tr. (.••tmir thr mt*»ult ttfUtf rtr^r. «• mUi »/ H%Htti»mr. nhunt Itut fr*» tkirK iUtt-H-lf*! «M •*• W*###»P»* . t h' *ffrflr* •(/ !*»> '^iifr'r-N ftfftfi,** tit th*' Vnrkrt- iftt-ttHl'f nm h4irf ^rttritiHf .1 itfrthtffMtr-tfff ftrikr. thf $ ftitifty 'tffi #••*«»/ •>***tftfrfmu ttf. tfi'i4tf*/ fftt't tillif thf mtr**t*t k''» {/«*'*•• 'A' m*-.*4ltU$t„* tht^f rktt^rtn; fnj H»M a§*ft in tnnttff rr»f»^rtm tk*-ft '•^^"fnkt^ i/** U4tt'kjf V>'- ' ttiiut nf mantttftn #(i«M«>iri r** r*-ifti'tt t.f Intrrr •^Irrtt-ttuH htirtt^ftHtf tk' limt"kf* ii uml^rlmu hft %tMatl tt^tnri,, if nffam n/ tti**i*'.tr r<"-k f *'JM-r * rftnrrfitts <■*•«* Trrtmrt/ uy ik»-m^ nrkm • f*rt**r4fH»/ttt muft •MnWof »*•#«, tk-lrm nnri t t.t»iiluinr-r*itrmi \ h^itm «#■»• -ttk*r h»trit»nl*tt .•/• pt-rtfttt M»*rf»*V«/»»Hi. I f tr*it^r»f*t ^urii^H ' fh* Mtnrkt'Msir uinttHtminm. f h^H »/' iVam nrr- •r«*« *- - < mi r^rtffW A f'^tr milt-m krttitr Mk^mat rnwaM. Tk^ •*-•> i^ • tut rrrngtm frwm fr^«MNi:A m Ihirk twnf «/ rnHgimmfr- pmt^nHa fmr takmnt »» miUm nnrtk »/ Mt»mtU tt^lth mamttHiU^^ rmrkm dij^ mtmtk : tk-4r «■)»<• iu ut^nfr,. prmhmkip uttd^Hir I fip^r famkHmn r^^Aw #^r^/i.. mmmmtmtH* mt-nr Smttu rirt-r. T',^ /»i44fmt»,if ti » • d^arwndimg ard^r mf thf mtna*« in tk^ u^tfgkk^»fl. •Tf oHttr«p:— Hrvwn, m*itmf^*nts mt§Htlp mt*tt'-i» i'um0i»mfrmt^ n^nuiUitr, eimrmrtff IntuiuHt^t trtth rfff miliri-itum mlnttt iir^ft, r*ttH/»mri ditl«9Hitf tm IM7.t th* #f^«W kmr* mt thr mouth nf t'inin > < •fvw wmrkmt fww pmtd mmd tfi^ldi-d pay nt Ihr i;f $». • dmp. Im itM dUtrihmtittm th^ ptlarp'r gnlii (• . f^M/lfMNi tm thm mrmm •(■Mf«>W«i> 9*M ^ mimttml mittrnp* ftrrmfnt tm Ik*- mtrmtm gmr. i thim »r9u. Thm fmmtry kma k*rm kr-nrilj/ ylnrint' i . prmhmkU thmt mtufk «/ tkr ymtd tknl •■j-tmtfH .... dmrim^ pr^0tm* rnitr^tttttitifj . mtr^nimM. #^i»«> ffi* . , n.itul in Ik*- yr^".- rir#r/'r««M fHrnt/tkHt rrm^k It. I'uknn, amti un „. »mtmit atrramtm fmlmrtmp frvtm Jtr mnulk. So rtmtm, k^fofk h*i~ ^*-i« foumd tm Ihtt rryittn. Tkf kwMt t— VmUp are S^ttrefm Hoolf ritrnttH nn't Ifntttr rif-'-, purtiam of tkf 6«r« trhen- tk*^ »♦•/*' i» rnttrfHt.n*. pitmnikim,trtik /n-tpt-r mppltnnrt-m, t» trnnk nut •tUtnti S. kmt Ihm rmfirkrtt p^rtinttm of the tntrm nrt- Mtittlh.u ltm*ii^ mrt^mt. f>;i. Ike hep tkm ■• im fke 'J.IHf, I, turn ftk- ■mtm. .riul • fktm :t ia ork rtml kii» <« <•/ vHl, Mr -jpa "/ ISS'stf Jl 125o 124°! N'.'10f>» 'N .1887. AJ888. 1902. ^,1904. l»07. imts. H»». H. To lu ifHiity R,p„rt A'o. l()!>7 £n,,fifA •out JTu. lom Fiervrh/