Williams Cone is a satellite cone of Mount Edziza, located 36 km (22 mi) 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 volcanic complex. Williams Cone last erupted about 1,350 years ago along with other nearby volcanoes, such as the well-preserved Eve Cone.[1]
| Williams Cone | |
|---|---|
  Williams Cone Location in British Columbia | |
| Highest point | |
| Elevation | 2,080 m (6,820 ft) |
| Prominence | 90 m (300 ft) |
| Coordinates | 57°46′48.0″N 130°35′56.4″W / 57.780000°N 130.599000°W |
| Geography | |
| Location | British Columbia, Canada |
| District | Cassiar Land District |
| Topo map | NTS 104G15 Buckley Lake |
| Geology | |
| Rock age | Holocene |
| Mountain type | Cinder cone |
| Volcanic arc/belt | Northern Cordilleran Volcanic Province |
| Last eruption | 1350 BP (600 CE) |
See also
editReferences
edit- ^ Catalogue of Canadian volcanoes: Williams ConeRetrieved on 2007-10-14 Archived 2007-11-10 at the Wayback Machine
External links
edit | This article related to a mountain, mountain range, or peak in British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |