Ray Mountain
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| Ray Mountain | |
|---|---|
| Elevation | 2,050 m (6,726 ft) |
| Location | |
| Location | British Columbia, Canada |
| Range | Shuswap Highland |
| Coordinates | 52°23′N 120°12′W / 52.383°N 120.2°W |
| Geology | |
| Type | Subglacial mound |
| Age of rock | Pleistocene |
| Volcanic arc/belt | Wells Gray-Clearwater volcanic field |
| Last eruption | Pleistocene |
Ray Mountain is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Ray Mountain last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field.
Lava from a conical vent on the southwest side of Ray Mountain flowed down Falls Creek for 6 or more miles almost to the outlet of Clearwater Lake.
[edit] See also
- Wells Gray-Clearwater volcanic field
- List of volcanoes in Canada
- Volcanism of Canada
- Volcanism of Western Canada
- Fissure vent
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