| Tuber Hill | |
|---|---|
  Tuber Hill Location in British Columbia | |
| Highest point | |
| Elevation | 2,500 m (8,200 ft) |
| Coordinates | 50°54′N123°24′W / 50.900°N 123.400°W /50.900; -123.400 |
| Geography | |
| Location | Upper Bridge River,British Columbia, Canada |
| Parent range | Pacific Ranges |
| Topo map | NTS92J14Dickson Range |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Stratovolcano |
| Volcanic arc | Canadian Cascade Arc |
| Volcanic belt | Garibaldi Volcanic Belt |
| Volcanic field | Bridge River Cones |
| Last eruption | Pleistocene |
Tuber Hill is a small 600,000-year-oldbasalticstratovolcano that was constructed on theBridge River highlands when nearby valleys were packed with ice. Tuber Hill is part of theGaribaldi segment of theCanadian Cascade Arc, but is not in the geographicCascade Range.
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