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 | |
|---|---|
  Armadillo Peak Location within British Columbia | |
| Highest point | |
| Elevation | 2,210 m (7,250 ft)[1][2] |
| Prominence | 405 m (1,329 ft)[2] |
| Listing | Volcanoes of Canada |
| Coordinates | 57°32′17″N 130°33′36″W / 57.53806°N 130.56000°W[3] |
| Geography | |
| Location | British Columbia, Canada |
| District | Cassiar Land District |
| Parent range | Tahltan Highland |
| Topo map | NTS 104G10 Mount Edziza[3] |
| Geology | |
| Age of rock | 7.5 million years |
| Mountain type | Caldera |
| Last eruption | Miocene[4] |
See also
editReferences
edit- ^ "Topographic map of Armadillo Peak". opentopomap.org. Retrieved 2023-06-14.
- ^ a b "Armadillo Peak". Bivouac.com. Retrieved 2023-06-14.
- ^ a b "Armadillo Peak". BC Geographical Names. Retrieved 2023-06-14.
- ^ "Armadillo Peak". Catalogue of Canadian volcanoes. Archived from the original on 2011-07-16.
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