Mount Sloan
Northeast aspect
Highest point
Elevation2,720 m (8,924 ft)[1]
Prominence500 m (1,640 ft)[1]
Parent peakMount Vayu (2,794 m)[2]
Isolation11.75 km (7.30 mi)[2]
ListingMountains of British Columbia
Coordinates50°46′55″N 122°58′18″W / 50.78194°N 122.97167°W / 50.78194; -122.97167[3]
Geography
Mount Sloan is located in British Columbia
Mount Sloan
Mount Sloan
Location in British Columbia
Mount Sloan is located in Canada
Mount Sloan
Mount Sloan
Mount Sloan (Canada)
CountryCanada
ProvinceBritish Columbia
DistrictLillooet Land District
Parent rangeThiassi Range
Coast Mountains
Topo mapNTS 92J15 Bralorne[3]
Climbing
Easiest routeScrambling (class 3)[4]

Mount Sloan is a 2,720-metre (8,924-foot) mountain summit located in British Columbia, Canada.

Description

Mount Sloan is the sixth-highest peak in the Thiassi Range which is a subrange of the Coast Mountains.[1] The remote mountain is situated 50 km (31 mi) north of Pemberton and 11 km (7 mi) west of the historic gold-mining community of Bralorne. Precipitation runoff from the peak drains north to Downton Lake which is a reservoir of the Bridge River. Mount Sloan is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 1,960 meters (6,430 ft) above Downton Lake in 5 km (3.1 mi). Mount Penrose rises to the north on the opposite side of the lake.

Etymology

The mountain was presumably named after David Sloan who was a mining engineer and managing director at the Pioneer Mine just east of Bralorne. He died on August 4, 1935, from injuries received in a floatplane crash at Alta Lake on July 30, 1935.[5] The crash also took the lives of the pilot, William R. McCluskey, Reginald Walter Brock and his wife Mildred. The mountain's toponym was officially adopted September 6, 1951, by the Geographical Names Board of Canada.[3]

Climate

Based on the Köppen climate classification, Mount Sloan is located in a subarctic climate zone of western North America.[6] 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.

See also

References

  1. 1 2 3 "Mount Sloan, British Columbia". Peakbagger.com. Retrieved 2022-12-03.
  2. 1 2 "Mount Sloan, Peakvisor.com". Retrieved 2022-12-03.
  3. 1 2 3 "Mount Sloan". Geographical Names Data Base. Natural Resources Canada. Retrieved 2022-12-03.
  4. ↑ Matt Gunn (2004), Scrambles in Southwest British Columbia, Cairn Publishing, ISBN 9780973548907.
  5. ↑ "Mount Sloan". BC Geographical Names. Retrieved 2022-12-03.
  6. ↑ 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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