geo.wikisort.org - MountainsPhillipps Peak is located on the border of Alberta and British Columbia on the Continental Divide. It was named in 1915 after Michael Phillipps who in 1873 was the first white man to cross Crowsnest Pass.[1] It is the lower west peak of Mount Tecumseh.
Geology
Phillipps Peak 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 during the Laramide orogeny.[2]
Climate
Based on the Köppen climate classification, Phillipps Peak has an alpine subarctic climate with cold, snowy winters, and mild summers.[3] Temperatures can drop below −20 °C with wind chill factors below −30 °C.
See also
- List of peaks on the Alberta–British Columbia border
- Mountains of Alberta
- Mountains of British Columbia
References
- PeakFinder
- Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
- 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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Ranges | |
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Mountains | |
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Passes |
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Glaciers |
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Rivers | |
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Peoples |
- Mountain Stoney
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Parks and protected areas | International |
- Canadian Rocky Mountain Parks World Heritage Site
- Waterton Biosphere Reserve
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National |
- Parks
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Provincial (AB) |
- Parks
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Provincial (BC) |
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Ski resorts |
- Castle Mountain
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- Fortress Mountain
- Lake Louise
- Little Mac
- Marmot Basin
- Mount Norquay
- Nakiska
- Powder King
- Sunshine Village
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Communities | |
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Ecozone and ecoregions |
- CEC ecozones
- Boreal Cordillera
- Montane Cordillera
- WWF ecoregions
- Alberta Mountain forests
- Alberta–British Columbia foothills forests
- North Central Rockies forest
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- See also
- Geography portal
- Canada portal
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