Cinder Mountain
From Wikipedia, the free encyclopedia
| Cinder Mountain | |
|---|---|
| Elevation | 300 m (984 ft) |
| Location | British Columbia, Canada |
| Range | Coast Mountains |
| Coordinates | |
| Type | Cinder cone |
| Age of rock | Pleistocene |
| 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 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.
[edit] See also
 |
This article about a location in British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
