Redoubt_Mountain

Redoubt Mountain

Redoubt Mountain

Mountain in Banff NP, Alberta, Canada


Redoubt Mountain (alternatively Mount Redoubt) is a mountain located in Banff National Park, in the Canadian Rockies of Alberta, Canada. It forms the southern buttress of Boulder Pass.

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The mountain was named in 1908 by Arthur O. Wheeler, founding member of the Alpine Club of Canada (AAC), as it resembled a redoubt (an outer military defense).[1]

The mountain can be climbed on a moderate to difficult scrambling route on the northwestern ridge.[5]

Like other mountains in Banff Park, it is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.[6] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[7]

Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers.[8] Temperatures can drop below -20 °C with wind chill factors below -30 °C.

See also


References

  1. "Redoubt Mountain". cdnrockiesdatabases.ca. Retrieved 2007-08-31.
  2. Lake Louise & Yoho (Map). 1:50,000. Cochrane, AB: Gem Trek Publishing. 2001. § B5. ISBN 1-895526-15-9. Retrieved 2019-06-11.
  3. "Redoubt Mountain". Bivouac.com. Retrieved 2009-01-02.
  4. Kane, Alan (1999). "Mount Redoubt". Scrambles in the Canadian Rockies. Calgary: Rocky Mountain Books. p. 255. ISBN 0-921102-67-4.
  5. Belyea, Helen R. (1960). The Story of the Mountains in Banff National Park (PDF). parkscanadahistory.com (Report). Ottawa: Geological Survey of Canada. Archived (PDF) from the original on 2015-10-02. Retrieved 2019-09-13.
  6. Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
  7. Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.

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