E NOTES

waters, ia near ble by small l'hr geuteunu of the eastern portion « } " the mouth © “= nl , ' ris ins, f on Mount Srku on (rat

coméllen is narigableus fn hilis ofthe Mackenele, differs in many res) ” l'elly. Small boats or ranors that totherwestirard, Heavily bedied Limestonr

Pelln jor at lrast 1NK0 miles sandstones and conglomerates, mostlis ivvath ny

h ortage at Hoole and Wolj colour e e preraili r “. Can )

on lake és the Limit of bout ETES D sian aile were found ut à » dber © “ ovw but in high stages, John oo, 1 ssl jorsns joint, Che nv tin , is s be renached LIT PAT + I rusyxe De | r Les of surifft water, vciths « CRT ET) 1 } ion n ton “… APT | are portage The Cravel “ net él one | alétr ivh be lortt / : ‘ 6°? dt from Laichu brook to the 1 ds 1 «idi / dis 1 «st 100 ia ä tater but it is prartically ntiuided in sundstone upriver lh : of the enstern por n oj the We ie

Gi Y. ntains havre genrral : northireczterly atrike ‘

rating dip being southrccsterti Fautting an ñ dest in the region and which the ntrate has gir-u t mountains their ch ic ,occur long the prrrt oj tie fovons and in many reaperts then ressemble the Hocks » western corner 0j the map tuins southern Canale

pare and do not appear to

uthivest on Finlauson rire The region of Lower elecation bordéring ER NOT Pr à is mndestlain bu small detached areas of Mrauzoi

mentary types dut largely Upper Cretuccous and Tertinry ge These + , tenture aid à svhist principatly sojt sandstonvra, shalrs ans conglomera h

ù dark grey or gr. eniaé Leds 41 either horisontal or gentliy tenédulatiresy } jus ren or! 1

es and attthe rocks are cut Tertiary beda rontain xereral aeams of ligrite.