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Re'surnd On southern Leith Ridge a variety of deformed and undeformed granitoid intrusions cu t deformed sillimanitemelt-bearing paragneisses. In the Hottah Lake-Fishtrap Lake area rocks of the Hottah Terrane a r e mostly cordieritebearing paragneisses intruded by foliated plutons. The plutons a re unconformably overlain by sedimentary and volcanic rocks of the MacTavish Supergroup and the supracrustal section was intruded by plutons of the Great Bear Batholith. Dans la partie sud de la cre'te Leith, une gamme d'instrusions granitoides de'forme'es e t non de'form6es traversent des paragneiss a sillimanite de'forme's. Dans la re'gion des lac Hottah e t Fishtrap, les roches du terrain de Hottah comprennent surtout des paragneiss a cordie'rite coupe's par des plutons feuillete's. Ces plutons reposent en discordance sous des roches se'dimentaires e t volcaniques du supergroupe de MacTavish; les plutons du batholite de Great Rear ont fa i t intrusion dans la section supe'rieure de la crodte.

Geology of the early proterozoic rocks in parts of the Leith Peninsula map area, District of Mackenzie