Great Bear Lake
A lake of central mainland Northwest Territories, Canada. The Great Bear River, about 113 km (70 mi) long, flows westward from the lake to the Mackenzie River.
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A lake of central mainland Northwest Territories, Canada. The Great Bear River, about 113 km (70 mi) long, flows westward from the lake to the Mackenzie River.
For more information on Great Bear Lake, visit Britannica.com.
| Great Bear Lake | |
|---|---|
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Map
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| Coordinates | |
| Primary outflows | Great Bear River |
| Catchment area | |
| Basin countries | Canada |
| Surface area | |
| Average depth | 72 m (236 ft) |
| Max depth | 446 m (1,463 ft) |
| Water volume | 2,236 km³ (536 mi³) |
| Shore length1 | 2,719 km (1,690 mi) |
| Surface elevation | 186 m (610 ft) |
| Settlements | Deline, Echo Bay |
| 1 Shore length is not a well-defined measure. | |
Great Bear Lake (Slavey: Sahtú, French: Grand lac de l'Ours) is the largest lake entirely within Canada (Lake Superior and Lake Huron straddling the Canada-US border are larger), the third largest in North America, and the seventh largest in the world.[1] The lake is situated on the Arctic Circle between 65 and 67 degrees of northern latitude and between 118 and 123 degrees western longitude, 186 m (610 ft) above sea level.
The lake has a surface area of
The lake empties through the Great Bear River (Sahtúdé) into the Mackenzie River. The only community on the lake is Deline, Northwest Territories at the southwest end.
The Sahtú Dene people took their name from the lake.
Great Bear Lake lies between two major physiographic regions: the Kazan Uplands portion of the Canadian Shield and the Interior Plains. Originally it was part of preglacial valleys that were reshaped by erosional effects of ice during the Pleistocene. Since then, the lake has undergone various changes resulting from rebound following the melting of the ice.
Precambrian rocks of the Canadian Shield form the eastern margin of the McTavish Arm. These rocks of the Precambrian are made up of sedimentary and metamorphic deposits supplemented by igneous intrusions forming dikes and sills.
Between 1950 and 1974, this climatic data was collected at Port Radium:
| Month | Temperature (°C) |
Precipitation (mm) |
Bright sunshine (hours) |
|---|---|---|---|
| Jan | –27.0 | 11 | 0.19 |
| Feb | –27.0 | 8 | 1.82 |
| Mar | –19.1 | 14 | 7.57 |
| Apr | –10.7 | 6 | 16.03 |
| May | +1.2 | 14 | 21.76 |
| Jun | +9.0 | 14 | 23.16 |
| Jul | +12.0 | 35 | 18.54 |
| Aug | +10.6 | 43 | 11.97 |
| Sep | +5.3 | 25 | 6.20 |
| Oct | –3.2 | 27 | 2.85 |
| Nov | –14.8 | 25 | 0.39 |
| Dec | –23.0 | 14 | 0.00 |
| Average | –7.2 | 10 | |
| Total | 236 |
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Dansk (Danish)
n. - Great Bear Lake
Deutsch (German)
n. - Größer Bären-See
עברית (Hebrew)
n. - ימת גרייט בר
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![]() | Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved. Read more | |
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![]() | Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/ Read more | |
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