This article needs additional citations for verification. (February 2021) |
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.[1]
| Cinder Mountain | |
|---|---|
| Highest point | |
| Elevation | 300 m (980 ft) |
| Coordinates | 56°34′N 130°37′W / 56.57°N 130.61°W |
| Geography | |
| Location | British Columbia, Canada |
| Parent range | Boundary Ranges |
| Geology | |
| Age of rock | Pleistocene |
| Mountain type | Cinder cone |
| Last eruption | Pleistocene |
See also edit
References edit
- ^ Geological Survey of Canada, Open File 2225. Natural Resources Canada. pp. 40–. GGKEY:1R1WRWJJ0YU.
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |