SOURCES OF INK
Laplorations and Geologv bd:
wW
Map compilation by:
sum be renchetd, ji miles of norift
ls are portique Dot [roms Enichu tah tretter brut it à
at up river
Lou)
oidest in the regio
lun, wecur alor th
wthicestern corne:
hi aveu aid dun
wuthicent on L'ént
ivres anti lranics
edimentary types
se torture and a sta oj « durk greu
detien ciad lt the
na are mate up shatlun sluitss y jrums | p} pré oj the t Ne aci mn the € “toner, crosses l'ell rtendéng in it l'rcvoat caño { be ! f{ néimitlar mountains, Thes thass oi e grapt r LE] LED (h mi the greuter } in range, tn y about 26 fret Uu river l'he strurd by am,
higher mountai
nite and doubtiesx
ps ouwve their w portion of the mant minor d at ravionx an ts «œuhote, theory ia rvéose There
similar bed
tion, may À
DRMATION
M. Dawson, 44 G. M Conuell .
Keele, 2902, 7:
. Ogilvie, 2886
Keele, /906.
in high at ” ’ th Hrt 1 . 4 U . n : / !
surift we th ‘ Lu e } url The ivre ‘ ‘ : : .
on Toiche brook to th t . P + 100 ” Gi u tte hist it ie ' , into ivre Lu t t ant "m port . d !
masntaine have generally « morthueastertu # ing dip being sonthreesterty. Fauiléng (1 in the region and whirh th = t us giren th proureotes d se h l or larg the put 0j the is nl bn intiny rraprcts the reet t Q terre corner 0j the mu} tuins . pers Cursus a and not appeur to cest on L'énlarnmun , The region ef ire ed fertng fe ed RAR TC ER ue + tendetrs bus amatl detachset ares of Mira ‘ Ru spas EU lrerts Upper Cretacrous and Tertinry y These + re dd à srhbistore pri: soft sundstones, ahuales nil conglonmme rs Le dark grey or greenish beds ar rithe Lorésontal &r gentliy rnmdulatiney } sut ait a s dré sut Tertiary beils rontain several sramas of tignit FUONOMIC NOTES made up mains of Indications of the presence of minerais of e «. slutrs inirpest verve trithin the trarereel partie Ed : ’ Mavkenvie minruntains 4 bed of iron ore un #ern uw lp ambrian te Grnvet à feu lon belote Shetal caen. The ocre bed sut j { he ti ces ete ing crops jroum b th on thirk one 0j conglomerale which i mr Gravel river, es£tende jor ahont 20 miles north 0j Mount bielthor LE companied by quartiites associatel rocks dip no th: their age is unknown but they k rh refrrr to us chert probably vndertis Epprer Cum CET hs rrposrud the ge ureve jou tn ack monntainn meur Nath rives ri vuriaiig ÉS UE me on dr } à ten belote Joht lake LI desrending order ef the stratua bn neiuhihonrhoet the lntunse, fiv uartz n re onttero} crosses l'elly virer in the Hrorrmn i CAPTTETEL stat 1,100 nding in « northereat Cong tle ti revoat non un Mur Hemuatit DATRITE 4 t «1j milarrochks crosses L ‘4 144 . Thesr ’ ka tre Gore t {t dolor (4 1,00% 4 graptolite beuringy Lu INT the gravel bars at the month 0f Finlanson rer an. Chert brecrina, CNT ked for gold and mietdrd pan at the rate SS. to he greuter } rt ©] some L EL [PTE An its distrit ion the ph rage is 1 ‘ n orange, Grid à fete {« njined to 1h + plaire À ’ . i P “ta host 20 fret in thickness thtt li , ha l'el an Hire! + rirers f el er lhesedinientir y PIN LI 1 st clins n PPT ire the : [ - 4 T2 y small badirs of hisereu. Th n 14 à heurily ylari { « Fr mountain peuks are probable the sai 7 volt that erintedl où k nd doubtless many other luring pre-glurial Lines has been distributed in th lat « «ce their height and drift The flise hu cote chéeh crrirhens th ver bars, has been derived from this drift by the enncentrating «ct 07 strains Fine gotit “ b ‘ ul in the ur DE] lelly tion of the Mackenzie river from Corn ilre reek to tt uk nel on netrat he ny minor deviations, « snnll streams entering from tir soutl Vo un un avious angles either to re khan been finit tn RE Er The beat bars th choie, they are broadly i ire bertireen Hoole canon nud Hoolr rit Oh tue #4 There is evidence port à « the bars chere he gold is roncentrat in similar beds with, orer posait eith proper appliances, to iraxh out ubout $3 14 n, may br to rer but the enviched portions of the hars are shallos C7:
léméttert ertent
125 30 125 vo: 1240
