Big Raven Plateau | |
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Coordinates: 57°42′49″N 130°45′06″W / 57.71361°N 130.75167°W[1] | |
Location | British Columbia, Canada |
Range | Tahltan Highland[2] |
Part of | Mount Edziza complex[3] |
Topo map | 104G10 Mount Edziza[1] |
Designation | Mount Edziza Provincial Park[2] |
The Big Raven Plateau is a lava plateau
Geography and geomorphology edit
Location edit
Cassiar Land District
Tahltan Highland
Mount Edziza volcanic complex
Structure edit
Mount Edziza
Mess Creek Escarpment
Landforms edit
Mount Edziza edit
Desolation Lava Field edit
Sleet Cone
Storm Cone
Triplex Cones
Sidas Cone
Twin Cone
Moraine Cone
Eve Cone
Williams Cone
Snowshoe Lava Field edit
Tennena Cone
Coffee Crater
Cocoa Crater
Keda Cone
The Saucer
Isolated landforms edit
Hoia Bluff
Kaia Bluff
Camp Hill
Cartoona Peak
Tsekone Ridge
Kana Cone
Drainage edit
Geology edit
Background edit
Northern Cordilleran Volcanic Province
Composition edit
Stratigraphy edit
Raspberry Formation
Armadillo Formation
Nido Formation (Tenchen Member)
Ice Peak Formation
Klastline Formation
Big Raven Formation
Basement edit
Stikinia
Human history edit
Yukon Telegraph Trail
Mount Edziza Provincial Park
Accessibility edit
See also edit
References edit
- ^ a b "Big Raven Plateau". BC Geographical Names. Archived from the original on 2021-09-30. Retrieved 2024-03-14.
- ^ a b Telegraph Creek, Cassiar Land District, British Columbia (Topographic map) (3 ed.). 1:250,000. A502 (in English and French). Department of Energy, Mines and Resources. 1989. Archived from the original on 2021-05-02. Retrieved 2021-09-25.
- ^ Souther 1992, p. 32.
Sources edit
- Souther, J. G. (1992). The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia. Geological Survey of Canada. doi:10.4095/133497. ISBN 0-660-14407-7.
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