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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 ...
The Laurentide ice sheet (LIS) was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glaciation epochs, from 2.58 million years ago to the present.
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 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 volumetric change of the Peyto Glacier, Alberta, Canada, 1896-1996 (M.A. thesis). Wilfrid Laurier University. CBC News (2003-01-10). "Prairies losing out on water from melting glacier" Munro, D. Scott. "Temperature trends in the Peyto Glacier weather station record" (PDF). Archived from the original (PDF) on June 5, 2007
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 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.
Lake Agassiz (/ ˈ æ ɡ ə s i / AG-ə-see) was a large proglacial lake that existed in central North America during the late Pleistocene, fed by meltwater from the retreating Laurentide Ice Sheet at the end of the last glacial period.
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