- Page 1 and 2:
Bulletin 48 Landforms of British Co
- Page 3 and 4:
The technical references are believ
- Page 5 and 6:
PAGE Chapter II.-Physiographic Subd
- Page 7 and 8:
FIQ. ILLUSTRATIONS 1. Landform map
- Page 9 and 10:
PLATE PAOE XVIII. (33) Stikine Plat
- Page 11 and 12:
PLATE XXXVIIB. (70) Rocky Mountain
- Page 13 and 14:
traveller. If he SO wishes, his enj
- Page 15 and 16:
pendants which, because of their se
- Page 17 and 18:
As Iava cools and consolidates, it
- Page 19 and 20:
are lithologic differences from pla
- Page 21 and 22:
mentary rocks are folded and faulte
- Page 23 and 24:
Field work by members of the Geolog
- Page 25 and 26:
BIBLIOGRAPHY Alden, W. C.: “ Phys
- Page 27 and 28:
The western boundary of the Eastern
- Page 29 and 30:
INSULAR MOUNTAINS The Insular Mount
- Page 31 and 32:
H. C., “ Geology and Mineral Depo
- Page 33 and 34:
The extreme northeastern tip of Gra
- Page 35 and 36:
the strait. It is suggested that th
- Page 37 and 38:
The lowland consists of many low, w
- Page 39 and 40:
anges farther west. The ranges sout
- Page 41 and 42:
Pacific Ranges The Pa&c Ranges (see
- Page 43 and 44:
Columbia. The mountains along the 4
- Page 45 and 46:
ones, and widening and deepening th
- Page 47 and 48:
south end of Teslin Lake, which sep
- Page 49 and 50:
Between the Taku &nd Sheslay Rivers
- Page 51 and 52:
The tuyas consist of nearly horizon
- Page 53 and 54:
sloping areas of upland remain undi
- Page 55 and 56:
mostly in the Babine Range. The roc
- Page 57 and 58:
to Eutsuk Lake on the southern side
- Page 59 and 60:
I These valleys are at a fairly hig
- Page 61 and 62:
Detailed studies made around severa
- Page 63 and 64:
The area is drained by the Finlay,
- Page 65 and 66:
Plateau and the Nechako Plateau, an
- Page 67 and 68:
iver in pre-Pl&ocene time or whethe
- Page 69 and 70:
dissected upland surface of the pla
- Page 71 and 72:
Thompson and North Thompson River v
- Page 73 and 74:
Adams, and Shuswap Rivers and their
- Page 75 and 76:
highlands, but the main effects of
- Page 77 and 78:
eda Rivers on the west and the Colu
- Page 79 and 80:
The amount of relief is governed by
- Page 81 and 82: “ 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 135 and 136: Tetsa River, topogrq Thenatlodi Mou