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Hoodoo Mountain | |
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Highest point | |
Elevation | 1,850 m (6,070 ft)[1] |
Prominence | 900 m (3,000 ft)[2] |
Listing | Mountains of British Columbia |
Dimensions | |
Length | 6 km (3.7 mi)[2] |
Width | 6 km (3.7 mi)[2] |
Volume | 17.3 km3 (4.2 cu mi)[3] |
Geography | |
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| |
Country | Canada[1] |
Province | British Columbia[1] |
District | Cassiar Land District[4] |
Parent range | Boundary Ranges[1] |
Topo map | NTS 104B14 Hoodoo Mountain[4] |
Geology | |
Rock age | < 85,000 yrs[5] |
Mountain type | Stratovolcano[3] |
Rock type(s) | Phonolite and trachyte[5] |
Volcanic region | Northern Cordilleran Province[3] |
Last eruption | 7050 BCE (?)[6] |
- ^ a b c d "Hoodoo Mountain: General Information". Global Volcanism Program. Smithsonian Institution. Archived from the original on 2021-03-18. Retrieved 2021-05-08.
- ^ a b c Wood, Charles A.; Kienle, Jürgen (2001). Volcanoes of North America: United States and Canada. Cambridge University Press. p. 127. ISBN 0-521-43811-X.
- ^ a b c Edwards, Benjamin R.; Russell, James K. (2000). "Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada". Geological Society of America Bulletin. 112 (8). Geological Society of America: 1280, 1281, 1283, 1284, 1286, 1287, 1291. Bibcode:2000GSAB..112.1280E. doi:10.1130/0016-7606(2000)112<1280:dnaoon>2.0.co;2. ISSN 0016-7606.
- ^ a b Cite error: The named reference
BCGN
was invoked but never defined (see the help page). - ^ a b Edwards, B. R.; Russell, J. K.; Anderson, R. G. (2002). "Subglacial, phonolitic volcanism at Hoodoo Mountain volcano, northern Canadian Cordillera". Bulletin of Volcanology. 64 (3–4). Springer-Verlag: 253–259, 261–264. Bibcode:2002BVol...64..254E. doi:10.1007/s00445-002-0202-9. ISSN 0258-8900. S2CID 73656495.
- ^ "Hoodoo Mountain: Eruptive History". Global Volcanism Program. Smithsonian Institution. Archived from the original on 2021-03-31. Retrieved 2021-05-08.