Cloudcroft Peaks
Climate
Cloudcroft Peaks is located in an alpine subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.
Geology
Like the other mountains in Glacier National Park, Cloudcroft Peaks 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.
Gallery
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East aspect -
Aerial view, circa 1925
See also
References
- ^ "Cloudcroft Peaks, Montana". Peakbagger.com. Retrieved August 2, 2017.
- ^ "Cloudcroft Peaks". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved August 2, 2017.
- ^ Mount Saint Nicholas, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved December 28, 2018.
- ^ 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.
- ^ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".
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