Mount Bell (Alberta) Explained

Mount Bell
Elevation M:2910
Elevation Ref:[1]
Prominence M:445
Prominence Ref:[2]
Isolation Km:2.58
Range:Bow Range
Canadian Rockies
Parent Peak:Mount Temple (3,544 m)[3]
Listing:Mountains of Alberta
Region Type:Province
Region:Alberta
Part Type:Protected area
Part:Banff National Park
Map:Canada Alberta#Canada
Map Size:260
Label Position:right
Coordinates:51.2842°N -116.1011°W
Coordinates Ref:[4]
Age:Cambrian
First Ascent:1910
Easiest Route:Scramble[5]

Mount Bell is a 2910m (9,550feet) summit in Alberta, Canada.

Geography

Mount Bell is set within Banff National Park, in the Bow Range of the Canadian Rockies.[3] The hamlet of Lake Louise is situated 16km (10miles) to the north and the Continental Divide is 4km (02miles) to the west. The nearest higher neighbor is Bident Mountain, 2.9km (01.8miles) to the west.[3] Bident Mountain forms the west buttress of Consolation Pass with Mount Bell forming the east buttress. These two peaks rise above the head of Consolation Valley. Precipitation runoff from Mount Bell drains into tributaries of the Bow River. Topographic relief is significant as the north aspect rises over above Taylor Lake in one kilometre (0.6 mile) and the south aspect rises above Boom Lake in two km (1.2 mile). The peak is visible from the Icefields Parkway to the east.

History

Originally called Mount Bellevue, the name was changed to honor Dr. Frederick Bell (1883–1971), a founding member of the Alpine Club of Canada and club president from 1926 through 1928.[1] [6] Mount Bell in British Columbia is also named after him. The mountain's toponym was officially adopted on April 3, 1952, by the Geographical Names Board of Canada.[4]

The first ascent of the summit was made in 1910 by an Alpine Club of Canada party including Nora Bell, sister of Frederick Bell.[7]

Geology

Like other mountains in Banff Park, Mount Bell 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.[8]

Climate

Based on the Köppen climate classification, Mount Bell is located in a subarctic climate zone with cold, snowy winters, and mild summers.[9] Winter temperatures can drop below with wind chill factors below .

See also

External links

Notes and References

  1. Glen W. Boles, William Lowell Putnam, Roger W. Laurilla (2006), Canadian Mountain Place Names: The Rockies and Columbia Mountains, Rocky Mountain Books,, p. 40.
  2. 2023-02-28.
  3. Web site: Mount Bell, Peakvisor.com. 2023-02-28.
  4. IAEDF. Mount Bell. 2023-02-28.
  5. Book: Kane, Alan. 2016. Scrambles in the Canadian Rockies. 3rd. Rocky Mountain Books. 9781771600972. 296.
  6. https://books.google.com/books?id=lpKie5RvQCAC&dq=Frederick+Bell+alpine+club+president+1926&pg=PT206 William Lowell Putnam, Andrew J. Kauffman (1986), The Guiding Spirit, Light Technology Publishing, LLC
  7. 108. Mount Bell. 2023-02-28.
  8. Book: Geology of the Rocky Mountains and Columbias . Gadd, Ben . 2008.
  9. Peel, M. C. . Finlayson, B. L. . McMahon, T. A. . amp . 2007 . Updated world map of the Köppen−Geiger climate classification . Hydrol. Earth Syst. Sci. . 11 . 5 . 1633–1644 . 10.5194/hess-11-1633-2007 . 2007HESS...11.1633P . 1027-5606. free .