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Waterton Lakes National Park Cameron Falls weather station has a humid continental climate (Koppen: Dfb), bordering relatively closely on a subarctic climate (Dfc). Summertime is mild with cool nights, while winter is chilly with highs around freezing. Snowfall is heavy, averaging 481.5 cm (189.6 inches). [27]
Mount Boswell is a 2,454-metre (8,051-foot) summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. It is situated along the east shore of Waterton Lake, one kilometre north of the Canada–United States border. Its nearest higher peak is Miche Wabun Peak, 5.0 km (3.1 mi) to the southeast. [1]
Waterton Park, commonly referred to as Waterton, is a hamlet in southwestern Alberta, Canada within Improvement District No. 4 Waterton (Waterton Lakes National Park). [3]It is located at the southwestern terminus of Highway 5, approximately 54 kilometres (34 mi) west of the Town of Cardston and 55 kilometres (34 mi) south of the Town of Pincher Creek.
Vimy Peak is a 2,385-metre (7,825-foot) summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada.It is set along the east shore of Waterton Lake on the opposite side from Waterton Park townsite.
The northern, lower end of the main lake lies in Waterton Lakes National Park while the upper, southern part of the lake is located in Glacier National Park. In 1979, UNESCO established the Waterton Biosphere Reserve to protect the diverse habitats including prairie grasslands, aspen parkland, subalpine forests, alpine tundra and freshwater ...
Mount Crandell is a 2,381-metre (7,812-foot) mountain summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. It is situated immediately north of the Waterton townsite. Its nearest higher peak is Bertha Peak, 2.94 km (1.83 mi) to the south-southwest. [5]
Waterton Biosphere Region (established 1979) is a UNESCO Biosphere Reserve encompassing Waterton Lakes National Park in the extreme southwest of the Province of Alberta, Canada. The region includes a section of the east slopes of the Rocky Mountains extending from the Continental Divide to the edge of the Canadian Great Plains to the east ...
Like other mountains in Waterton Lakes National Park, Mount Blakiston is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny.