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silverhorn+mountain Latitude and Longitude:

51°45′45″N 116°29′56″W / 51.76250°N 116.49889°W / 51.76250; -116.49889
From Wikipedia, the free encyclopedia
Silverhorn Mountain
Silverhorn Mountain, south aspect
Highest point
Elevation2,911 m (9,551 ft) [1]
Prominence168 m (551 ft) [1]
Parent peak Observation Peak (3174 m) [1]
Listing Mountains of Alberta
Coordinates 51°45′45″N 116°29′56″W / 51.76250°N 116.49889°W / 51.76250; -116.49889 [2]
Geography
Silverhorn Mountain is located in Alberta
Silverhorn Mountain
Silverhorn Mountain
Location of Silverhorn Mountain in Alberta
Silverhorn Mountain is located in Canada
Silverhorn Mountain
Silverhorn Mountain
Silverhorn Mountain (Canada)
Location Banff National Park
Alberta, Canada
Parent rangeMurchison Group
Canadian Rockies
Topo map NTS 82N16 Siffleur River [2]
Geology
Age of rock Cambrian
Type of rock Sedimentary
Climbing
Easiest route Scrambling

Silverhorn Mountain is a 2,911-metre (9,551-foot) mountain summit located in the Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Silverhorn Mountain is situated 3.9 kilometres southeast of Mount Weed, and 3.1 km northwest of Observation Peak. Silverhorn stands directly east across the Mistaya River valley from Mount Patterson, and both are prominent features seen from the Icefields Parkway.

History

The mountain was given its descriptive name in 1899 by Rev. Charles Lathrop Noyes (1851-1923), a member of the Appalachian Mountain Club who climbed in the Rockies and made several first ascents, such as Mount Balfour, Mount Gordon, and Mount Lefroy. [1] The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. [2]

Geology

Like other mountains in Banff Park, Silverhorn is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. [3] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. [4]  

Climate

Based on the Köppen climate classification, Silverhorn Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. [5] Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Silverhorn Mountain drains west into the Mistaya River, or east into Dolomite Creek which is a tributary of the Siffleur River.

See also

References

  1. ^ a b c d "Silverhorn Mountain". Bivouac.com. Retrieved 2019-09-06.
  2. ^ a b c "Silverhorn Mountain". Geographical Names Data Base. Natural Resources Canada. Retrieved 2019-09-06.
  3. ^ 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.
  4. ^ Geology of the Rocky Mountains and Columbias, by Ben Gadd, 2008
  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: 1633–1644. ISSN  1027-5606.

External links


silverhorn+mountain Latitude and Longitude:

51°45′45″N 116°29′56″W / 51.76250°N 116.49889°W / 51.76250; -116.49889
From Wikipedia, the free encyclopedia
Silverhorn Mountain
Silverhorn Mountain, south aspect
Highest point
Elevation2,911 m (9,551 ft) [1]
Prominence168 m (551 ft) [1]
Parent peak Observation Peak (3174 m) [1]
Listing Mountains of Alberta
Coordinates 51°45′45″N 116°29′56″W / 51.76250°N 116.49889°W / 51.76250; -116.49889 [2]
Geography
Silverhorn Mountain is located in Alberta
Silverhorn Mountain
Silverhorn Mountain
Location of Silverhorn Mountain in Alberta
Silverhorn Mountain is located in Canada
Silverhorn Mountain
Silverhorn Mountain
Silverhorn Mountain (Canada)
Location Banff National Park
Alberta, Canada
Parent rangeMurchison Group
Canadian Rockies
Topo map NTS 82N16 Siffleur River [2]
Geology
Age of rock Cambrian
Type of rock Sedimentary
Climbing
Easiest route Scrambling

Silverhorn Mountain is a 2,911-metre (9,551-foot) mountain summit located in the Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Silverhorn Mountain is situated 3.9 kilometres southeast of Mount Weed, and 3.1 km northwest of Observation Peak. Silverhorn stands directly east across the Mistaya River valley from Mount Patterson, and both are prominent features seen from the Icefields Parkway.

History

The mountain was given its descriptive name in 1899 by Rev. Charles Lathrop Noyes (1851-1923), a member of the Appalachian Mountain Club who climbed in the Rockies and made several first ascents, such as Mount Balfour, Mount Gordon, and Mount Lefroy. [1] The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. [2]

Geology

Like other mountains in Banff Park, Silverhorn is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. [3] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. [4]  

Climate

Based on the Köppen climate classification, Silverhorn Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. [5] Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Silverhorn Mountain drains west into the Mistaya River, or east into Dolomite Creek which is a tributary of the Siffleur River.

See also

References

  1. ^ a b c d "Silverhorn Mountain". Bivouac.com. Retrieved 2019-09-06.
  2. ^ a b c "Silverhorn Mountain". Geographical Names Data Base. Natural Resources Canada. Retrieved 2019-09-06.
  3. ^ 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.
  4. ^ Geology of the Rocky Mountains and Columbias, by Ben Gadd, 2008
  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: 1633–1644. ISSN  1027-5606.

External links


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