Lone Walker Mountain (8,502 feet (2,591 m)) is located in the Lewis Range, Glacier National Park in the U.S. state of Montana.[3] Lone Walker Mountain is situated immediately southwest of Upper Two Medicine Lake along the Continental Divide.
Lone Walker Mountain | |
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Highest point | |
Elevation | 8,502 ft (2,591 m)[1] |
Prominence | 822 ft (251 m)[1] |
Coordinates | 48°27′12″N 113°28′44″W / 48.45333°N 113.47889°W[2] |
Geography | |
Location | Flathead County, Montana, Glacier County, Montana, U.S. |
Parent range | Lewis Range |
Topo map | USGS |
Climate
editBased on the Köppen climate classification, it is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.[4] Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Geology
editLike other mountains in Glacier National Park, it 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]
See also
editReferences
edit- ^ a b "Lone Walker Mountain, Montana". Peakbagger.com. Retrieved December 26, 2018.
- ^ "Lone Walker Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved December 26, 2018.
- ^ Mount Rockwell, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved December 26, 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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