Split Mountain | |
---|---|
Highest point | |
Elevation | 8,797 ft (2,681 m)[1] |
Prominence | 1,272 ft (388 m)[1] |
Parent peak | Norris Mountain (8,882 ft)[2] |
Isolation | 1.50 mi (2.41 km)[2] |
Coordinates | 48°35′53″N 113°32′21″W / 48.59806°N 113.53917°W[3] |
Geography | |
Split Mountain Location in Montana Split Mountain Location in the United States | |
Location | Glacier National Park Glacier County, Montana, U.S. |
Parent range | Lewis Range |
Topo map | USGS Mount Stimson, MT |
Climbing | |
First ascent | 1956[1] |
Easiest route | class 5+[2] |
Split Mountain (8,797 feet (2,681 m)) is located in the Lewis Range, Glacier National Park in the U.S. state of Montana.[4]
Geology
Like other mountains in Glacier National Park, Split Mountain 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.[5]
Climate
Based on the Köppen climate classification, it is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.[6] Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Gallery
See also
References
- 1 2 3 "Split Mountain, Montana". Peakbagger.com. Retrieved December 27, 2018.
- 1 2 3 "Split Mountain - 8,792' MT". listsofjohn.com. Retrieved 2021-10-14.
- ↑ "Split Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved December 27, 2018.
- ↑ Mount Stimson, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved December 27, 2018.
- ↑ 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 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606. S2CID 9654551.