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10 relations: Arctic Ocean, Canada, Geological Survey of Canada, Great Bear Lake, Great Slave Lake, Lake Agassiz, Lake Athabasca, List of prehistoric lakes, Mackenzie River, Proglacial lake.
Arctic Ocean
The Arctic Ocean is the smallest and shallowest of the world's five major oceans.
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Canada
Canada is a country located in the northern part of North America.
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Geological Survey of Canada
The Geological Survey of Canada (GSC; Commission géologique du Canada (CGC)) is a Canadian federal government agency responsible for performing geological surveys of the country, developing Canada's natural resources and protecting the environment.
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Great Bear Lake
The Great Bear Lake (Slavey: Sahtú; Grand lac de l'Ours) is the largest lake entirely in Canada (Lake Superior and Lake Huron straddling the Canada–US border are larger), the fourth largest in North America, and the eighth largest in the world.
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Great Slave Lake
The Great Slave Lake (Grand lac des Esclaves) is the second-largest lake in the Northwest Territories of Canada (after Great Bear Lake), the deepest lake in North America at, and the tenth-largest lake in the world.
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Lake Agassiz
Lake Agassiz was a very large glacial lake in central North America.
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Lake Athabasca
Lake Athabasca (French: lac Athabasca; from Woods Cree: aðapaskāw, " there are plants one after another") is located in the northwest corner of Saskatchewan and the northeast corner of Alberta between 58° and 60° N. The lake is 26% in Alberta and 74% in Saskatchewan.
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List of prehistoric lakes
This a partial list of prehistoric lakes.
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Mackenzie River
The Mackenzie River (Slavey language: Deh-Cho, big river or Inuvialuktun: Kuukpak, great river; fleuve (de) Mackenzie) is the longest river system in Canada, and has the second largest drainage basin of any North American river after the Mississippi River.
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Proglacial lake
In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic depression of the crust around the ice.
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