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Thelon Wildlife Sanctuary

Thelon Wildlife Sanctuary
IUCN category Ib (wilderness area)
Thelon river oasis.jpg
The "oasis" section of the Thelon River, below Warden's Grove.
Location Northwest Territories and Nunavut, Canada
Coordinates 64°49′59″N 102°10′00″W / 64.83306°N 102.16667°W / 64.83306; -102.16667Coordinates: 64°49′59″N 102°10′00″W / 64.83306°N 102.16667°W / 64.83306; -102.16667
Area 52,000 square kilometres (20,077 sq mi)
Established 1927 (1927)
Governing body Nunavut Parks
http://www.nunavutparks.com/english/parks-special-places/thelon-wildlife-sanctuary/overview.aspx

The Thelon Wildlife Sanctuary, at 52,000 square kilometres (20,077 sq mi), over twice the area of Belgium, is the largest wildlife refuge in Canada. It is located in northern Canada's Arctic region, north of the tree line, straddling the Northwest Territories and Nunavut, halfway between Baker Lake and Yellowknife, and bordered on the north between the Baillie River on the west and the Consul River at the east by the Back River. It is the namesake of the Thelon River, whose river valley is resplendent with boreal forest biological diversity, hence its identification as a "Biological Site of Universal Importance" by the International Biological Program (IBP) in the 1960s.

Established in 1927 as the Thelon Game Sanctuary to conserve muskox populations, its original size was 39,000 square kilometres (15,000 sq mi). It was expanded in 1956 to its present size, and is home to the most northernly known moose above the tree line. In addition, the wildlife sanctuary is home to barren-ground caribou (Beverly and Bathurst herds), Arctic wolf, Arctic fox, wolverine, Arctic squirrel (sicsic), barren ground grizzly bear and waterfowl.

The "Thelon Oasis" is a section of the wildlife sanctuary along the Thelon River valley between Warden Grove (the Thelon's confluence with Hanbury River) and Hornby Point. Even though it is north of the Arctic tree line, the area supports thick white spruce tree groves, raspberry, currant, and columbine plants, along with tall alluvial dwarf willow thickets and tag alder. Scientists believe the causes of this unusual proliferation of plants more common to subarctic areas include favorable fine-textured soils and climatic oasis effect, higher summer temperatures due to northward elevation fall and the absence of large lakes.


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