Caribou Tuya
| Caribou Tuya | |
|---|---|
| File:Caribou Tuya.jpg | |
| Highest point | |
| Elevation | 1,770 m (5,810 ft) |
| Geography | |
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| |
| Location | British Columbia, Canada |
| Region | CA |
| Parent range | Tuya Range |
| Geology | |
| Mountain type | Subglacial mound |
| Volcanic arc/belt | Northern Cordilleran Volcanic Province |
| Last eruption | Pleistocene |
Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation (25 to 10 ka). Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward. Locally the sections are capped by subaerial basaltic lava flows. Samples of the glassy pillow basalts and hyaloclastites along with crystalline basalt flows were collected at Caribou Tuya. The volcano is believed to have formed and last erupted during the Pleistocene Epoch.[1]
See also
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Volcanism of Canada
- Volcanism of Western Canada
- Volcanic history of the Northern Cordilleran Volcanic Province
References
 | This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it. |
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |