Tuber Hill
Tuber Hill is a small 600,000-year-old basaltic stratovolcano that was constructed on the Bridge River highlands when nearby valleys were packed with ice. Tuber Hill is part of the Garibaldi segment of the Canadian Cascade Arc, but is not in the geographic Cascade Range.
| Tuber Hill | |
|---|---|
| Highest point | |
| Elevation | 2,500 m (8,200 ft) |
| Coordinates | 50°54′N 123°24′W |
| Geography | |
| Location | Upper Bridge River, British Columbia, Canada |
| Parent range | Pacific Ranges |
| Geology | |
| Age of rock | Pleistocene |
| Mountain type | Stratovolcano |
| Volcanic arc/belt | Canadian Cascade Arc Garibaldi Volcanic Belt |
| Last eruption | Pleistocene |
See also
References
- "Bridge River Cones". Global Volcanism Program. Smithsonian Institution.
- Catalogue of Canadian volcanoes - Tuber Hill
.svg.png.webp){kind=small}
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.