Mount Girouard

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Mount Girouard
Mts Inglismaldie Girouard.jpg
Mount Inglismaldie (left) and Mount Girouard (right)
Highest point
Elevation 2,995 m (9,826 ft) [1]
Prominence 1,455 m (4,774 ft) [2]
Listing Mountains of Alberta
Coordinates 51°14′10″N115°24′11″W / 51.23611°N 115.40306°W / 51.23611; -115.40306 [3]
Geography
Canada Alberta relief location map - transverse mercator proj.svg
Red triangle with thick white border.svg
Mount Girouard
Location in Alberta
Country Canada
Province Alberta
Protected area Banff National Park
Parent range Fairholme Range
Topo map NTS 82O3 Canmore [3]
Climbing
First ascent 1938 by E.E. Bishop and D.R. Crosby [1] [2]
Easiest route rock climb

Mount Girouard is the highest peak of the Fairholme Range in Banff National Park, Alberta, Canada. Mt. Girouard is located in the Bow River valley south of Lake Minnewanka.

Contents

The mountain was named in 1904 after Sir Édouard Girouard, a railway builder in Africa during the rule of the British Empire. [1] [2]

Geology

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

Climate

Based on the Köppen climate classification, Mount Girouard is located in a subarctic climate with cold, snowy winters, and mild summers. [5] Temperatures can drop below −20 °C (−4 °F) with wind chill factors below −30 °C (−22 °F). Precipitation runoff from the mountain drains into the Bow River.

See also

Related Research Articles

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References

  1. 1 2 3 "Mount Girouard". cdnrockiesdatabases.ca. Retrieved 2004-09-29.
  2. 1 2 3 "Mount Girouard". Bivouac.com. Retrieved 2008-05-25.
  3. 1 2 "Mount Girouard". Geographical Names Data Base . Natural Resources Canada . Retrieved 2019-08-02.
  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 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007 . ISSN   1027-5606.