The Table (British Columbia)
| The Table | |
|---|---|
The Table rises above the southwest side of Garibaldi Lake | |
| Highest point | |
| Elevation | 2,021 m (6,631 ft) |
| Prominence | 251 m (823 ft) |
| Listing | Mountains of British Columbia |
| Coordinates | 49°53′42″N 123°00′47″W / 49.89500°N 123.01306°W |
| Geography | |
| Interactive map of The Table | |
| Location | British Columbia, Canada |
| District | New Westminster Land District |
| Parent range | Garibaldi Ranges |
| Topo map | NTS 92G14 Cheakamus River |
| Geology | |
| Rock age | Holocene |
| Mountain type | Tuya |
| Volcanic arc/belt | Canadian Cascade ArcGaribaldi Volcanic Belt |
| Last eruption | Holocene |
| Climbing | |
| First ascent | 1916 Tom Fyles |
The Table, sometimes called Table Mountain, is a 2,021-metre (6,631 ft) high flow-dominated andesite tuya located 4 kilometres (2 mi) south of Garibaldi Lake, 15 kilometres (9 mi) northeast of Cheekye and 5 kilometres (3 mi) north of Mount Garibaldi, British Columbia, Canada. It rises over 530 metres (1,740 ft) above the surface of Garibaldi Lake, which lies less than 1 kilometre (1 mi) to the north.
The Table is almost impossible to climb because sections of the volcano have collapsed, creating steep and exceptionally rotten rock walls on all sides.