Cinder Cone (British Columbia)
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| Cinder Cone | |
|---|---|
| Elevation | 1,910 m (6,266 ft) |
| Prominence | 120 m (394 ft) |
| Location | |
| Location | British Columbia, Canada |
| Range | Garibaldi Ranges |
| Coordinates | 49°58′18″N 123°00′25″W / 49.97167°N 123.00694°W |
| Topo map | NTS 92G/14 |
| Geology | |
| Type | Cinder cone |
| Age of rock | Holocene |
| Volcanic arc/belt | Cascade Volcanic Arc Garibaldi Volcanic Belt |
| Last eruption | Holocene |
Cinder Cone is a cinder cone with a small crater on the west side of the Helm Glacier in Garibaldi Provincial Park. Cinder Cone is surrounded by cinder flats and its crater is filled with melt water during the summer. Cinder Cone gets eroded easily by melt water during the spring, washing the pyroclastics into the Valley of Desolation. Cinder Cone produced a 9 km (6 mi) long lava flow during the early Holocene.
[edit] See also
[edit] References
- "Cinder Cone". BC Geographical Names. http://apps.gov.bc.ca/pub/bcgnws/names/670.html.
- "Cinder Cone". Bivouac.com. http://www.bivouac.com/MtnPg.asp?MtnId=594.
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