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Bulletin 48 Landforms of British Co
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The technical references are believ
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PAGE Chapter II.-Physiographic Subd
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FIQ. ILLUSTRATIONS 1. Landform map
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PLATE PAOE XVIII. (33) Stikine Plat
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PLATE XXXVIIB. (70) Rocky Mountain
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traveller. If he SO wishes, his enj
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pendants which, because of their se
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As Iava cools and consolidates, it
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are lithologic differences from pla
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mentary rocks are folded and faulte
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Field work by members of the Geolog
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BIBLIOGRAPHY Alden, W. C.: “ Phys
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The western boundary of the Eastern
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INSULAR MOUNTAINS The Insular Mount
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H. C., “ Geology and Mineral Depo
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The extreme northeastern tip of Gra
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the strait. It is suggested that th
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The lowland consists of many low, w
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anges farther west. The ranges sout
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Pacific Ranges The Pa&c Ranges (see
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Columbia. The mountains along the 4
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ones, and widening and deepening th
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south end of Teslin Lake, which sep
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Between the Taku &nd Sheslay Rivers
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The tuyas consist of nearly horizon
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sloping areas of upland remain undi
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mostly in the Babine Range. The roc
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to Eutsuk Lake on the southern side
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I These valleys are at a fairly hig
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Detailed studies made around severa
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The area is drained by the Finlay,
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Plateau and the Nechako Plateau, an
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iver in pre-Pl&ocene time or whethe
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dissected upland surface of the pla
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Thompson and North Thompson River v
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Adams, and Shuswap Rivers and their
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highlands, but the main effects of
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eda Rivers on the west and the Colu
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The amount of relief is governed by
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“ Striae, roches moutonn&s, and l
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