Cloudraker Mountain

Cloudraker Mountain
North aspect centered on skyline, from Mt. Taylor
Highest point
Elevation	2,385 m (7,825 ft) [1] [2]
Prominence	674 m (2,211 ft) [1]
Parent peak	Skihist Mountain [2]
Isolation	12.09 km (7.51 mi) [1]
Listing	Mountains of British Columbia
Coordinates	50°05′42″N122°26′26″W / 50.09500°N 122.44056°W / 50.09500; -122.44056 [3]
Geography
Cloudraker Mountain Location in British Columbia Show map of British Columbia Cloudraker Mountain Location in Canada Show map of Canada
Interactive map of Cloudraker Mountain
Location	British Columbia, Canada
District	New Westminster Land District
Parent range	Coast Mountains [1] Lillooet Ranges [2]
Topo map	NTS 92J1 Stein Lake
Climbing
First ascent	1967
Easiest route	Northeast Ridge class 3 [4]

Cloudraker Mountain is a 2,385-metre (7,825-foot) glaciated summit in British Columbia, Canada.

Description

Cloudraker Mountain is located in the Lillooet Ranges of the Coast Mountains, 37 kilometres (23 mi) southeast of Pemberton and 37 kilometres (23 mi) east of Whistler. Precipitation runoff and glacial meltwater from this mountain drains into tributaries of the Lillooet River. Cloudraker Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 935 metres (3,070 ft) above Tao Lake in less than two kilometres (1.2 mi) and 2,185 metres (7,170 ft) above Lillooet Lake in seven kilometres (4.3 mi). The mountain's toponym was officially adopted March 31, 1969, by the Geographical Names Board of Canada. ^[3] The mountain's name was submitted by climber Christian Adam whose party made the first ascent of the summit on August 1, 1967. ^[3] He wrote that the peak's twin summits project through their common glacier and reach up into the clouds.

Climate

Based on the Köppen climate classification, Cloudraker Mountain is located in the marine west coast climate zone of western North America. ^[5] 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. This climate supports an unnamed glacier on the north slope of the peak. The months July through September offer the most favorable weather for climbing Cloudraker Mountain.

See also

• Mountains portal

• Geography of British Columbia
• Geology of British Columbia

References

1. "Cloudraker Mountain, British Columbia". Peakbagger.com. Retrieved 2024-03-03.
2. "Cloudraker Mountain, Peakvisor.com" . Retrieved 2024-03-03.
3. "Cloudraker Mountain". BC Geographical Names .
4. "Cloudraker Mountain". Bivouac.com. Retrieved 2024-03-03.
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. Bibcode:2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007 . ISSN   1027-5606.

External links

• Weather: Cloudraker Mountain