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Athabasca Glacier, Jasper National Park, Alberta.. A comprehensive list of glaciers in Canada began with glacial surveys by the Water Survey of Canada (WSC) from 1945 to 1980, [1] including an inventory begun for the International Geophysical Year (1957–58) and contributions to the World Glacier Inventory (WGI, now part of the World Glacier Monitoring Service) for the International ...
It was up to 2 mi (3.2 km) thick in Nunavik, Quebec, Canada, but much thinner at its edges, where nunataks were common in hilly areas. It created much of the surface geology of southern Canada and the northern United States, leaving behind glacially scoured valleys, moraines, eskers and glacial till. It also caused many changes to the shape ...
The Columbia Icefield is the largest ice field in North America's Rocky Mountains. [1] Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park.
The Athabasca Glacier is one of the six principal 'toes' of the Columbia Icefield, located in the Canadian Rockies.The glacier currently loses depth at a rate of about 5 metres (16 ft) per year [2] and has receded more than 1.5 km (0.93 mi) and lost over half of its volume in the past 125 years.
The Illecillewaet Glacier / ˌ ɪ l ə ˈ s ɪ l ə w ə t / is a glacier in British Columbia, Canada. It is located inside Glacier National Park in the Selkirk Mountains, a sub-range of the Columbia Mountains. After the construction of the Canadian Pacific Railway (CPR) near the glacier's terminus, and the building of a hotel nearby, the ...
The Agassiz Ice Cap formerly Agassiz Glacier [1] is an ice cap on the central eastern side of Ellesmere Island, Nunavut, Canada. [2] The Agassiz ice cap is about 21,000 km 2 (8,100 sq mi) in area. [2] It is located between the North Ellesmere ice field to the north and the Prince of Wales Icefield to the south.
The glacier is a primary water source for the North Saskatchewan River. The glacier is approximately 13 kilometres (8.1 mi) long and covers an area of 30 km 2 (11.5 mi 2 ) and was measured in 1960 to be over 400 metres (1,310 ft) thick at a distance of 8 kilometres (5.0 mi) from the terminal snout. [ 1 ]
The name of the glacier was suggested by the Geological Survey of Canada on November 15, 1979, and eventually became official on November 24, 1980. Tennaya is derived from the Tahltan words ten and naya, which mean ice and be come down respectively. The name of this glacier is a reference to a spectacular icefall at the head of Tennaya valley. [1]
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