Kaina Mountain (9,494 feet (2,894 m)) is located in the Lewis Range, Glacier National Park in the U.S. state of Montana.[3] Kaina Mountain is in the northeastern section of Glacier National Park and north of Kaina Lake.
Kaina Mountain | |
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Highest point | |
Elevation | 9,494 ft (2,894 m)[1] |
Prominence | 1,329 ft (405 m)[1] |
Coordinates | 48°57′14″N 113°47′56″W / 48.95389°N 113.79889°W[2] |
Geography | |
Location | Glacier County, Montana, U.S. |
Parent range | Lewis Range |
Topo map | USGS Mount Cleveland MT |
Climbing | |
First ascent | Unknown |
Easiest route | class 3-4 |
Climate
editBased on the Köppen climate classification, Kaina is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.[4] Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.
Geology
editLike other mountains in Glacier National Park, Kaina 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 "Kaina Mountain, Montana". Peakbagger.com. Retrieved May 28, 2018.
- ^ "Kaina Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved May 28, 2018.
- ^ Mount Cleveland, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved May 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: 1633–1644. ISSN 1027-5606.
- ^ Gadd, Ben (2008). Geology of the Rocky Mountains and Columbias.