Blackcomb Peak Explained

Blackcomb Peak
Elevation M:2436
Elevation Ref:[1]
Prominence M:86
Range:Fitzsimmons Range
Location:British Columbia, Canada
District:New Westminster Land District
Map:British Columbia#Canada
Map Size:250
Label Position:right
Coordinates:50.0814°N -122.8708°W
First Ascent:1923 by Phyllis Munday and Don Munday
Easiest Route:class 3

Blackcomb Peak (Ucwalmícwts: Tsíqten) is a mountain located east of Whistler, British Columbia that forms the boundary between the Whistler Blackcomb ski resort and Garibaldi Provincial Park. Like Whistler Mountain, it is located on the edge of Garibaldi Provincial Park and the ski lifts are often used to access the park, particularly for the Spearhead Traverse.

Several ski runs are established on the mountain, with Whistler Village at the base of the mountain on the side facing Whistler Mountain, and Blackcomb Village below the opposite face. The 2010 Winter Olympics sliding sports including Bobsleigh, Luge and Skeleton[2] took place on its slopes, at the Whistler Sliding Centre located on it.

Climate

Based on the Köppen climate classification, Blackcomb Peak is located in the marine west coast climate zone of western North America.[3] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Blackcomb Peak.

See also

Gallery

External links

Notes and References

  1. 635. Blackcomb Peak. 2007-02-18.
  2. Web site: Whistler Sliding Centre. Whistler Sliding Centre . June 25, 2024.
  3. 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 . 1027-5606.