Bishops Cap
Geology
Like other mountains in Glacier National Park, Bishops Cap 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
According to the Köppen climate classification system, Bishops Cap is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer.
Gallery
See also
References
- ^ "Bishops Cap, Montana". Peakbagger.com. Retrieved June 4, 2018.
- ^ "Bishops Cap - 9,127' MT". listsofjohn.com. Retrieved 2021-11-05.
- ^ "Bishops Cap". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved June 4, 2018.
- ^ Logan Pass, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved June 4, 2018.
- ^ Holterman, Jack (2006). Place Names of Glacier National Park. Helena, MT: Riverbend Publishing. p. 34. ISBN 1-931832-68-4.
- ^ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".
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(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. ISSN 1027-5606.