The Castle is a lava spine located west of Squamish in southwestern British Columbia, Canada. Volcanism at The Castle is controlled by north–south structures and there are no hot springs known in the area.[2] It forms part of the Monmouth Creek complex and is part of the Garibaldi Volcanic Belt which is a segment of the Cascade Volcanic Arc.
| The Castle | |
|---|---|
| Highest point | |
| Elevation | 510 m (1,670 ft)[1] |
| Prominence | 40 m (130 ft)[1] |
| Listing | Mountains of British Columbia |
| Coordinates | 49°41′N 123°11′W[1] |
| Geography | |
| Location | British Columbia, Canada |
| District | New Westminster Land District |
| Parent range | Pacific Ranges |
| Topo map | NTS 92G11 Squamish |
| Geology | |
| Age of rock | Pleistocene |
| Mountain type | Lava spine |
| Volcanic arc/belt | Canadian Cascade ArcGaribaldi Volcanic Belt |
| Last eruption | Pleistocene |
Volcanoes of the Garibaldi Volcanic Belt | |
|---|---|
|
This article about a location on the Coast of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |