Salal Glacier volcanic complex
| Salal Glacier volcanic complex | |
|---|---|
| Highest point | |
| Elevation | 2,400 m (7,900 ft) [1] | 
| Coordinates | 50°47′N 123°23′W / 50.79°N 123.38°W | 
| Geography | |
| Location | British Columbia, Canada | 
| Parent range | Pacific Ranges | 
| Geology | |
| Age of rock | 970,000 years | 
| Mountain type | Complex volcano | 
| Volcanic arc/belt | 
Canadian Cascade Arc Garibaldi Volcanic Belt  | 
| Last eruption | 590,000 years | 
The Salal Glacier volcanic complex is a complex volcano in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located near the upper Bridge River. It is part of a volcanic group called the Bridge River Cones which in turn is part of the Garibaldi Volcanic Belt of the Canadian Cascade Arc.[2]
See also
References
- ↑ "Bridge River Cones". Global Volcanism Program. Smithsonian Institution. Retrieved 2010-03-12.
 - ↑ "Salal Glacier". Catalogue of Canadian volcanoes. Geological Survey of Canada. 2009-03-10. Retrieved 2010-03-12.
 
This article is issued from Wikipedia - version of the Friday, June 21, 2013. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.