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Rainbow Mountain (British Columbia)

Coordinates: 50°10′47″N 123°03′13″W / 50.17972°N 123.05361°W / 50.17972; -123.05361
From Wikipedia, the free encyclopedia
Rainbow Mountain
Southwest aspect, seen from Tricouni Peak
Highest point
Elevation2,314 m (7,592 ft)[1]
Prominence1,019 m (3,343 ft)[1]
Parent peakMount Callaghan[1]
Coordinates50°10′47″N 123°03′13″W / 50.17972°N 123.05361°W / 50.17972; -123.05361[2]
Geography
Rainbow Mountain is located in British Columbia
Rainbow Mountain
Rainbow Mountain
Location in British Columbia
Rainbow Mountain is located in Canada
Rainbow Mountain
Rainbow Mountain
Location in Canada
Map
Interactive map of Rainbow Mountain
CountryCanada
ProvinceBritish Columbia
DistrictNew Westminster Land District
Parent rangeGaribaldi Ranges
Topo mapNTS 92J3 Brandywine Falls
Climbing
Easiest routeScramble

Rainbow Mountain is a broad glaciated mountain forming the northeastern wall of the Callaghan Valley in the Pacific Ranges of British Columbia, Canada. Located in the middle of the Sea to Sky Country, the mountain is just 9 km (5.6 mi) northwest of the resort town of Whistler, and is a popular destination for hiking, snowshoeing and ski touring.

Climate

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Based on the Köppen climate classification, Rainbow Mountain 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. Winter 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 c "Rainbow Mountain". Bivouac.com. Retrieved 5 April 2015.
  2. ^ "Rainbow Mountain". BC Geographical Names. Retrieved 5 April 2015.
  3. ^ Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN 1027-5606.
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