| Round Mountain | |
|---|---|
  Round Mountain Location in British Columbia | |
 | |
| Interactive map of Round Mountain | |
| Highest point | |
| Elevation | 1,646 m (5,400 ft) |
| Prominence | 225 m (738 ft) |
| Coordinates | 49°45′53.5″N123°01′27.1″W / 49.764861°N 123.024194°W /49.764861; -123.024194 |
| Geography | |
| Location | British Columbia,Canada |
| District | New Westminster Land District |
| Parent range | Garibaldi Ranges |
| Topo map | NTS 92G14Cheakamus River |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Outcrop |
| Last eruption | Pleistocene |
| Climbing | |
| Easiest route | gravel road |
Round Mountain is an erodedvolcanic outcrop in theGaribaldi Volcanic Belt inBritish Columbia,Canada, located 8 km southwest of Eanastick Meadows, 9 km (6 mi) east ofBrackendale and 10 km (6 mi) south ofMount Garibaldi. It is the highpoint ofPaul Ridge and is located in the southwest corner ofGaribaldi Provincial Park. Round Mountain formed as a result ofsubduction of theJuan de Fuca Plate beneath theNorth American Plate, known as theCascadia subduction zone. Round Mountain last erupted during thePleistocene.
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