Trolltinder Mountain
Trolltinder Mountain seen from Iceline Trail
Highest point
Elevation2,912 m (9,554 ft)[1]
Prominence112 m (367 ft)[1]
ListingMountains of British Columbia
Coordinates51°33′26″N 116°28′55″W / 51.55722°N 116.48194°W / 51.55722; -116.48194[2]
Geography
Trolltinder Mountain is located in British Columbia
Trolltinder Mountain
Trolltinder Mountain
Location of Trolltinder Mountain in British Columbia
Trolltinder Mountain is located in Canada
Trolltinder Mountain
Trolltinder Mountain
Trolltinder Mountain (Canada)
LocationYoho National Park
British Columbia, Canada
DistrictKootenay Land District
Parent rangeWaputik Range
Canadian Rockies
Topo mapNTS 82N9 Hector Lake[2]
Geology
Age of rockCambrian
Type of rockSedimentary
Climbing
First ascent1901 J. Outram, E. Whymper, C. Kaufmann, C. Klucker, J. Pollinger[1]
Easiest routeClimbing Class 5[1]

Trolltinder Mountain is a 2,912-metre (9,554-foot) mountain summit located immediately west of the Continental Divide, in the Waputik Range of the Canadian Rockies in British Columbia, Canada.[1] It is situated in Yoho National Park, with its nearest higher peak being Mount Balfour, 1.0 km (0.62 mi) to the northeast, and Fairy Lake directly below its southern slope.[1]

History

The mountain was named by Jean Habel in 1897 for its resemblance to a mountain in Norway.[1] The translation is Witch's Peak.[3][4] Jean Habel was a German geographer who explored the Yoho Valley in 1896.[5]

The first ascent of the mountain was made in 1901 by James Outram and Edward Whymper, with guides Christian Kaufmann, Christian Klucker, and Joseph Pollinger.[6] Outram described the climb in his book, "In the Heart of the Canadian Rockies" as follows: "On the 21st we had a little climb to a ruined tower on a serrated spur of Mt. Balfour, which had been called by Mr. Habel "Trolltinder," or the Witch's Peaks, after a famous and much pinnacled ridge above the Romsdal in Norway: the legend saying that the points represent a wedding party turned to stone by an evil genius. It was an absurdly simple climb, though somewhat laborious, except for the last fifty feet, which gave us a really good gymnastic scramble." [7]

The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada.[2]

Geology

Trolltinder Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.[8] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[9]

Climate

Based on the Köppen climate classification, Trolltinder Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers.[10] Temperatures can drop below −20 °C with wind chill factors below −30 °C.

See also

References

  1. 1 2 3 4 5 6 7 "Trolltinder Mountain". Bivouac.com. Retrieved 2019-03-31.
  2. 1 2 3 "Trolltinder Mountain". Geographical Names Data Base. Natural Resources Canada. Retrieved 2019-03-31.
  3. ↑ "Trolltinder Mountain". BC Geographical Names. Retrieved 2019-09-23.
  4. ↑ Chambers' Encyclopædia: A Dictionary of Universal Knowledge, page 796
  5. ↑ W., Boles, Glen (2006). Canadian mountain place names : the Rockies and Columbia Mountains. Laurilla, Roger W., 1959-, Putnam, William Lowell., Putnam, William Lowell. Place names of the Canadian Alps. Calgary, Alta.: Rocky Mountain Books. ISBN 9781894765794. OCLC 244770225.{{cite book}}: CS1 maint: multiple names: authors list (link)
  6. ↑ "Trolltinder Mountain". cdnrockiesdatabases.ca. Retrieved 2019-09-23.
  7. ↑ In the Heart of the Canadian Rockies, James Outram, Rocky Mountain Books, 2007
  8. ↑ Belyea, Helen R. (1960). The Story of the Mountains in Banff National Park (PDF). parkscanadahistory.com (Report). Ottawa: Geological Survey of Canada. Archived (PDF) from the original on 2015-10-02. Retrieved 2019-09-13.
  9. ↑ Gadd, Ben (2008). Geology of the Rocky Mountains and Columbias.
  10. ↑ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.
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