Pharaoh Peaks

Pharaoh Peaks is a 2,713-metre (8,901-foot) mountain with three summits located in Banff National Park in Alberta, Canada. Pharaoh Peaks are part of the Ball Range in the Canadian Rockies.[3] The nearest higher peak is Scarab Peak, 2.0 km (1.2 mi) to the southwest. The mountain's name Pharaoh was in keeping with the Egyptian theme of the immediate surrounding area, e.g., Egypt Lake, Pharaoh Lake, Mummy Lake, and Scarab Lake, which were applied in 1922 by Arthur O. Wheeler of the Interprovincial Boundary Survey.[1] Wheeler regarded the area particularly beautiful when he wrote: "After 30 years of exploration, surveys and mapping the main ranges of the Canadian Rockies, the writer ... can safely say that outstanding among them for scenic charm and interest may be classed the group of peaks, lakes and alpine meadows of the Egypt Lake area."[4] The mountain's name was officially adopted in 1956 when approved by the Geographical Names Board of Canada.[2]

Pharaoh Peaks
Pharaoh Peaks
Highest point
Elevation2,713 m (8,901 ft) [1]
Prominence410 m (1,350 ft) [1]
ListingMountains of Alberta
Coordinates51°06′32″N 115°54′43″W [2]
Geography
Pharaoh Peaks
Location of Pharaoh Peaks in Alberta
Pharaoh Peaks
Pharaoh Peaks (Canada)
LocationBanff National Park
Alberta, Canada
Parent rangeBall Range, Canadian Rockies
Topo mapNTS 82O/04[2]
Geology
Age of rockCambrian
Type of rockSedimentary rock
Climbing
Easiest routeScramble
Pharaoh Peaks from the Healy Pass area

Geology

Like other mountains in Banff Park, Pharaoh Peaks are composed of sedimentary rock laid down during the Precambrian to Jurassic periods.[5] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[6]

Climate

Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers.[7] Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb the mountain. Precipitation runoff from the mountain drains into tributaries of the Bow River.

See also

References
  1. "Pharaoh Peaks". Bivouac.com. Retrieved 2019-03-26.
  2. "Pharaoh Peaks". Geographical Names Data Base. Natural Resources Canada. Retrieved 2019-03-25.
  3. "Ball Range". Peakbagger.com. Retrieved 2019-03-27.
  4. Banff - Assiniboine: a beautiful world : a guide to the trails and the rich history of Banff National Park from Palliser Pass to Vermilion Pass, plus the core area of Mount Assiniboine Provincial Park by Don Beers, Highline Publishing, 1993.
  5. 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.
  6. Gadd, Ben (2008). Geology of the Rocky Mountains and Columbias.
  7. 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.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.