Burnside River | |
---|---|
Location | |
Country | Canada |
Territory | Nunavut |
Physical characteristics | |
Source | Contwoyto Lake |
• coordinates | 66°2′36″N111°14′33″W / 66.04333°N 111.24250°W |
• elevation | 444 m (1,457 ft) |
Mouth | Bathurst Inlet |
• location | Bathurst Inlet, Nunavut |
• coordinates | 66°51′N108°04′W / 66.850°N 108.067°W |
• elevation | 0 m (0 ft) |
Basin size | 16,800 km2 (6,500 sq mi) [1] |
Discharge | |
• average | 135 m3/s (4,800 cu ft/s) [1] |
• minimum | 46.8 m3/s (1,650 cu ft/s) [1] |
• maximum | 313 m3/s (11,100 cu ft/s) [1] |
The Burnside River is a river in the Canadian territory of Nunavut. It has its headwaters at Contwoyto Lake, flows across the Precambrian Shield's Contwoyto Plateau, flows through isolated and rugged tundra, into Lake Kathawachaga, and through the Wilberforce Hills region. Before emptying into Bathurst Inlet on the Arctic Ocean, the Mara River empties into the Burnside River. [2] The river has an island, Nadlak, historically notable for Inuit use of caribou antlers as hut roof infrastructures.
The river is surrounded by continuous permafrost. It is migratory crossing path of Bathurst barren-ground caribou. Wildlife includes Arctic wolf, grizzly bears and muskox, while birds include golden eagle, rough-legged hawk and gyrfalcon. Arctic char, Arctic grayling, lake trout, and whitefish are also found in the river. Plants along the shoreline include dwarf willow and alder, plus 125 different wild flowers. [3]
Copper Inuit artifacts and gravestones are located in the Burnside River area, along with trade items (needles, tools) they received from Dene. The area was explored in 1821 and 1822 by Sir John Franklin. [3] From 1930 to 1964, a Hudson's Bay Company trading post operated at the river's mouth where the community of Bathurst Inlet formed. [4] Present day, it is a popular wilderness whitewater canoe route, offering long stretches of continuous whitewater, as well as several more challenging sets of rapids. [3]
Over the period 1976 to 2022, the Burnside River has a mean flow of 135 cubic metres per second (4,800 cu ft/s). Mean minimal flow is 48.6 cubic metres per second (1,720 cu ft/s) and mean maximum flow is 313 cubic metres per second (11,100 cu ft/s). Record maximum flow was 995 cubic metres per second (35,100 cu ft/s) in June 2001, while record minimum flow was 0 cubic metres per second (0 cu ft/s) in April 1983. [1]
The Back River, formerly Backs River, is the 20th longest Canadian river and is located in the Northwest Territories and Nunavut. It rises at an unnamed lake in the North Slave Region of the Northwest Territories and flows more than 974 km (605 mi) mostly through the Kivalliq Region, Nunavut, to its mouth at the Arctic Ocean in the Kitikmeot Region of Nunavut.
Ukkusiksalik National Park is a national park in Nunavut, Canada. It covers 20,885 km2 (8,064 sq mi) of tundra and coastal mudflats south of the Arctic Circle and the hamlet of Naujaat, from Hudson Bay's Roes Welcome Sound towards the western Barrenlands and the source of Brown River. The park surrounds Wager Bay, a 100 km (62 mi)-long inlet on the Hudson Bay. Although the smallest of Nunavut's four national parks, it is the sixth largest in Canada. Its name relates to steatite found there: Ukkusiksalik means "where there is material for the stone pot".
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Bathurst Inlet, officially Kiluhiqtuq, is a deep inlet located along the northern coast of the Canadian mainland, at the east end of Coronation Gulf, into which the Burnside and Western rivers empty. The name, or its native equivalent Kingoak, is also used to identify the community of Bathurst Inlet located on the shore. Melville Sound opens into the eastern side of the inlet at Cape Croker, west of the Hurd Islands.
The Mara River is a river in Nunavut which flows into the Burnside River to empty into Bathurst Inlet on the Arctic Ocean. It flows north from headwaters at Nose Lake and is 260 kilometres (160 mi) long.
Bathurst Inlet, is a small Inuit community located in Bathurst Inlet in the Kitikmeot Region of Nunavut, Canada, at the mouth of the Burnside River.
The Coulonge River is a predominantly wilderness river in western Quebec, Canada.
The Kazan River, is a Canadian Heritage River located in Nunavut, Canada. The Dene name for the river was Kasba-tue meaning "white partridge river." The name was apparently changed to Kazan in the late 19th century due to the influence of Order of Mary Immaculate missionaries. The river headwaters are in northern Saskatchewan at Kasba Lake, and it flows north for about 1,000 kilometres (620 mi) before emptying into Baker Lake, on the opposite side of the mouth of the Thelon River. Along its course the river flows through several lakes, including Ennadai Lake and Yathkyed Lake, over the Kazan Falls, down a red sandstone gorge and through both boreal forest and tundra. It is the last section of the river, below Ennadai Lake, that is above the timber line and is designated a Canadian Heritage River.
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Copper Inuit, also known as Inuinnait and Kitlinermiut, are a Canadian Inuit group who live north of the tree line, in what is now the Kitikmeot Region of Nunavut and in the Inuvialuit Settlement Region in the Inuvik Region of the Northwest Territories. Most of them historically lived in the area around Coronation Gulf, on Victoria Island, and southern Banks Island.
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