Eve Cone
Eve Cone | |
---|---|
Highest point | |
Elevation | 1,702 m (5,584 ft) |
Prominence | 172 m (564 ft) |
Coordinates | 57°48′47″N 130°40′30″W / 57.813°N 130.675°W |
Geography | |
Location | Stikine Country, British Columbia, Canada |
District | Cassiar Land District |
Parent range | Tahltan Highland (southwestern Stikine Plateau) |
Topo map | NTS 104G15 |
Geology | |
Age of rock | Holocene |
Mountain type | Cinder cone |
Volcanic arc/belt | Northern Cordilleran Volcanic Province |
Last eruption | 700 |
Eve Cone is a well-preserved black cinder cone on the Big Raven Plateau, British Columbia, Canada. It is one of the 30 cinder cones on the flanks of the massive shield volcano of Mount Edziza that formed in the year 700, making it one of the most recent eruptions on the Big Raven Plateau and in Canada. Eve Cone stands by itself in the middle of the Desolation Lava Field and its distinctive shape can be seen from a long distance. Commonly photographed[citation needed], Eve Cone is covered by light yellow pumice from a close by but unknown vent.
See also[]
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Northern Cordilleran Volcanic Province
- Volcanism of Canada
- Volcanism of Western Canada
References[]
Categories:
- Cinder cones of British Columbia
- Northern Cordilleran Volcanic Province
- Stikine Country
- Holocene volcanoes
- Monogenetic cinder cones
- Tahltan Highland
- One-thousanders of British Columbia
- British Columbia Interior geography stubs