Armadillo Peak is a 7.5-million-year-old caldera, located about 3 km north of Bourgeaux Creek and northeast of Raspberry Pass, British Columbia, Canada. It is south of Mount Edziza and is overlapped by the Ice Peak central volcano, which was formed during the early Pleistocene. Its caldera is largely destroyed by glaciers. It is part of the Mount Edziza volcanic complex, which is made of basaltic lava flows.
Armadillo Peak | |
---|---|
Highest point | |
Elevation | 2,210 m (7,250 ft) |
Prominence | 405 m (1,329 ft) |
Coordinates | 57°32′17.9″N 130°33′36.0″W |
Geography | |
Location | British Columbia, Canada |
District | Cassiar Land District |
Parent range | Tahltan Highland |
Topo map | NTS 103G10 Griffith Harbour |
Geology | |
Age of rock | 7.5 million years |
Mountain type | Caldera |
Last eruption | Miocene |
![]() | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |