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Hoodoo Mountain
A flat-topped, snow-covered mountain rising over green-leafed trees on a clear day.
Hoodoo Mountain as seen from the Iskut River
Highest point
Elevation1,850 m (6,070 ft)[1]
Prominence900 m (3,000 ft)[2]
ListingMountains of British Columbia
Dimensions
Length6 km (3.7 mi)[2]
Width6 km (3.7 mi)[2]
Volume17.3 km3 (4.2 cu mi)[3]
Geography
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CountryCanada[1]
ProvinceBritish Columbia[1]
DistrictCassiar Land District[4]
Parent rangeBoundary Ranges[1]
Topo mapNTS 104B14 Hoodoo Mountain[4]
Geology
Rock age< 85,000 yrs[5]
Mountain typeStratovolcano[3]
Rock type(s)Phonolite and trachyte[5]
Volcanic regionNorthern Cordilleran Province[3]
Last eruption7050 BCE (?)[6]
  1. ^ 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.
  2. ^ 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.
  3. ^ 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.
  4. ^ a b Cite error: The named reference BCGN was invoked but never defined (see the help page).
  5. ^ 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.
  6. ^ "Hoodoo Mountain: Eruptive History". Global Volcanism Program. Smithsonian Institution. Archived from the original on 2021-03-31. Retrieved 2021-05-08.