Williams Cone
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| Williams Cone | |
|---|---|
| Elevation | 2,080 m (6,824 ft) |
| Location | British Columbia, Canada |
| Prominence | 90 m (295 ft) |
| Coordinates | |
| Topo map | NTS 104G/15 |
| Type | Cinder cone |
| Volcanic arc/belt | Northern Cordilleran Volcanic Province |
| Age of rock | Holocene |
| Last eruption | 1340 BP |
Williams Cone is a satellite cone of Mount Edziza, located 36 kilometers east of Telegraph Creek. It lies just off the northern edge of the Tencho Icefield and is one of the many postglacial cinder cones that lie on the Mount Edziza plateau. Williams Cone last erupted about 1,350 years ago along with other nearby volcanoes, such as the well-preserved Eve Cone.[1]
[edit] See also
[edit] References
- ^ Catalogue of Canadian volcanoes: Williams Cone Retrieved on 2007-10-14
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