Landforms of British Columbia 1976 - Department of Geography

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Quam Quartz ~ountam Queen Bess, Mount ~~~~~~~~ . -~~_~~...~~ _... 39 Queen Charlotte Islands, intrusive rock ~.. I6 sedimentary anp vo+ic rocks ..~ 20 Queen CharlotB Queen Charlotte M Queen Charlotte Rang< QWS” te! Hi: sedimentary rocks ..~~~~ ~..~ 17 selection <strong>of</strong> boundaries - - 24 Selkirk Mountains ..~.~~~~~ 78 136 Shulapr Shulaps Rang +uswap Fi Shuswap terrain, dip slopes - ~.~~.~ 21 ‘n.Creek :~~~ - - - 48 dO”“tai” - 44
Tetsa River, topogrq Thenatlodi Mountain Thiedemann. M Thomason Plate
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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
Page 83 and 84: The boundary between the Rocky Moun
Page 85 and 86: [References: Price, R. A., “ Fern
Page 87 and 88: 8,820 feet, and the lowest point in
Page 89 and 90: margin of the Rocky Mountains% it s
Page 91 and 92: Devonian limestones that are thrust
Page 93 and 94: locally, as a rule only on the nort
Page 95 and 96: Dept. of Mines and Petroleum Remmx?
Page 97 and 98: CHAPTER III.-SPECIAL ASPECTS OF THE
Page 99 and 100: movement, and regional studies of t
Page 101 and 102: Both the Atlas of British Columbia
Page 103 and 104: ase of the Sumas till in the Fraser
Page 105 and 106: British Columbia includes the drain
Page 107 and 108: The Parsnip and Finlay Rivers were
Page 109 and 110: upper Fraser River is the result of
Page 111 and 112: Its pattern of flow within the moun
Page 113 and 114: materials. Along the west coast of
Page 115 and 116: , Pleistocene probably has been bet
Page 117 and 118: A small volcanic cone with associat
Page 119 and 120: ‘I , titularly for those interest
Page 121 and 122: The Pinchi fault and its northweste
Page 123 and 124: component of the discordant pattern
Page 125 and 126: APPENDIX B.-GLOSSARY * Aggrade-to b
Page 127 and 128: Lineation-in rock the parallel orie
Page 129 and 130: INDEX The place names listed are th
Page 131: 85 126 :: :: 116
Page 136: 138
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Landforms of British Columbia 1976 - Department of Geography

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