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Wonder Peak

Coordinates: 50°53′41″N 115°33′31″W / 50.89472°N 115.55861°W / 50.89472; -115.55861
From Wikipedia, the free encyclopedia
Wonder Peak
Wonder Peak at sunset
Highest point
Elevation2,852 m (9,357 ft)[1]
Prominence165 m (541 ft)
Coordinates50°53′41″N 115°33′31″W / 50.89472°N 115.55861°W / 50.89472; -115.55861
Geography
Wonder Peak is located in Alberta
Wonder Peak
Wonder Peak
Location in Alberta and British Columbia
Wonder Peak is located in British Columbia
Wonder Peak
Wonder Peak
Wonder Peak (British Columbia)
LocationAlberta
British Columbia
Parent rangeCanadian Rockies
Topo mapNTS 82J13 Mount Assiniboine
Climbing
First ascent1913 Conrad Kain, Boundary Commission[2]

Wonder Peak is located on the border of Alberta and British Columbia in the Canadian Rockies. Situated on the Continental Divide, it also straddles the shared boundary of Banff National Park with Mount Assiniboine Provincial Park. It was named in 1913 by Arthur O. Wheeler and Conrad Kain.[1][2]

Geology

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Wonder Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.[3] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[4]

Climate

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Based on the Köppen climate classification, Wonder Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers.[5] Temperatures can drop below -20°C with wind chill factors below -30°C.

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See also

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References

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  1. ^ a b "Wonder Peak". cdnrockiesdatabases.ca. Retrieved 2019-09-16.
  2. ^ a b "Wonder Peak". Bivouac.com. Retrieved 2019-09-16.
  3. ^ 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.
  4. ^ Gadd, Ben (2008). Geology of the Rocky Mountains and Columbias.
  5. ^ 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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