| Ray Mountain | |
|---|---|
| Elevation | 2,050 m (6,726 ft) |
| Location | |
| Location | British Columbia, Canada |
| Range | Shuswap Highland |
| 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.