| Sofa Mountain | |
|---|---|
 North aspect | |
| Highest point | |
| Elevation | 2,515 m (8,251 ft) |
| Prominence | 38 m (125 ft) |
| Parent peak | Crypt Peak (2,615 m) |
| Isolation | 4.59 km (2.85 mi) |
| Coordinates | 49°01′17″N 113°47′09″W / 49.02139°N 113.78583°W / 49.02139; -113.78583 |
| Naming | |
| Etymology | Sofa (descriptive) |
| Geography | |
  Sofa MountainLocation in AlbertaShow map of Alberta Sofa MountainSofa Mountain (Canada)Show map of Canada
| |
| Interactive map of Sofa Mountain | |
| Location | Alberta, Canada |
| Parent range | Canadian Rockies Lewis Range |
| Topo map | NTS 82H4 Waterton Lakes |
| Geology | |
| Rock age | Cambrian |
| Rock type | Sedimentary rock |
| Climbing | |
| Easiest route | Scrambling Northeast Ridge |
Sofa Mountain is a 2,515-meter (8,251-foot) summit located in Waterton Lakes National Park, in Alberta, Canada. It is part of the Lewis Range which is a subset of the Canadian Rockies, and is the easternmost mountain in the Canadian Rockies, as well as the park. It is situated 5.4 km (3.4 mi) east of Vimy Peak, and the nearest higher neighbor is Crypt Peak, 4.6 km (2.9 mi) to the southwest. Topographic relief is significant as the north aspect rises over 1,220 meters (4,000 feet) above Middle Waterton Lake in approximately six kilometers (3.7 mi).
History
The mountain was named in 1865 by Kootenay Brown who wrote: "Coming down from the mountain, where we got our first glimpse of the buffalo, we soon reached the prairie shore of a large lake at the further side of which a mountain rose to a sofa-like peak among the clouds. This mountain was afterwards called Sofa Mountain." This mountain's name was officially adopted in 1943 by the Geographical Names Board of Canada.
Geology
Like other mountains in Waterton Lakes National Park, Sofa Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long over younger rock of the cretaceous period.
Climate
Based on the Köppen climate classification, Sofa Mountain has an alpine subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Sofa Mountain drains to the Waterton River and Belly River.
Gallery
-
Northwest aspect
See also
References
- ^ "Sofa Mountain, Alberta". Peakbagger.com. Retrieved 2021-10-16.
- Andrew Nugara, More Scrambles in the Canadian Rockies, 2014, Rocky Mountain Books, ISBN 9781771600163, page 87.
- ^ "Sofa Mountain". Geographical Names Data Base. Natural Resources Canada. Retrieved 2021-10-16.
- Andrew Nugara, More Scrambles in the Canadian Rockies, 2014, Rocky Mountain Books, ISBN 9781771600163, page 87.
- Dave Birrell, 50 Roadside Panoramas in the Canadian Rockies, Rocky Mountain Books, 2000, ISBN 9780921102656, page 151.
- "Sofa Mountain". cdnrockiesdatabases.ca. Retrieved 2021-10-16.
- Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".
{{cite journal}}: Cite journal requires|journal=(help) - 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): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606. S2CID 9654551.
External links
- Parks Canada web site: Waterton Lakes National Park
- Weather forecast: Sofa Mountain
| Places adjacent to Sofa Mountain | ||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| ||||||||||||||||
Sofa Mountain
