Cinder Mountain
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| Cinder Mountain | |
|---|---|
| Highest point | |
| Elevation | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
| Coordinates | Lua error in package.lua at line 80: module 'strict' not found. |
| Geography | |
| Location | British Columbia, Canada |
| Parent range | Boundary Ranges |
| Geology | |
| Age of rock | Pleistocene |
| Mountain type | Cinder cone |
| Last eruption | Pleistocene |
Cinder Mountain is a partly eroded cinder cone at the head of Snippaker Creek, British Columbia, Canada. It is one of the Iskut-Unuk River Cones and is the source of a basaltic lava flow that extends 4 km (2 mi) north into Copper King Creek. An isolated pile of subaerial basalt flows and associated pillow lava rest on varved clay and till in King Creek. Cinder Mountain last erupted during the Pleistocene.
See also
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Northern Cordilleran Volcanic Province
- The Volcano
- Volcanism of Canada
- Volcanism of Western Canada
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