Mount Saint Nicholas
Mount Saint Nicholas excels in terms of steep vertical relief, even by the high standards prevalent in Glacier National Park. For example, its northwest face rises one vertical mile (5,300 ft; 1,600 m) in approximately 1.5 horizontal miles (7,900 ft; 2.4 km). Due to its pointed shape and isolation from the Continental Divide, it has similarly precipitous drops in all directions.
In 1926, Reverend Conrad Wellen of Havre, Montana made the first ascent of Mount Saint Nicholas. The mountain had previously been considered by many to be unclimbable. The standard route is the Northeast Ridge. Starting from the east side of the peak, this route begins with a straightforward scramble up a gully to a prominent notch. From the notch a thousand vertical feet of somewhat technical climbing remain.
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.
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. Temperatures can drop below −10 °F with wind chill factors below −30 °F.
See also
References
- ^ "Mount Saint Nicholas, Montana". Peakbagger.com. Retrieved 2013-01-20.
- ^ "Mount Saint Nicholas". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2013-01-20.
- ^ Edwards, J. Gordon (1995). A Climber's Guide to Glacier National Park. Falcon Press.
- ^ Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
- ^ 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.
External links