Mount Henkel (8,774 feet (2,674 m)) is located in the Lewis Range, Glacier National Park in the U.S. state of Montana.[3] Kennedy Lake is just to the north of the mountain.
Geology
Like other mountains in Glacier National Park, the 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.[4]
Climate
Based on the Köppen climate classification, the peak is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.[5] Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Gallery
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Southwest aspect -
Grinnell Point, Mt. Wilbur, Mt. Henkel (right of center)
See also
References
- ^ a b "Mount Henkel, Montana". Peakbagger.com. Retrieved December 26, 2018.
- ^ "Mount Henkel". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved December 26, 2018.
- ^ Mount Henkel, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved June 15, 2018.
- ^ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".
{{cite journal}}: Cite journal requires|journal=(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 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606. S2CID 9654551.