Stony Lake | |
---|---|
Location | Division No. 23, North Manitoba |
Coordinates | 58°51′12″N98°38′09″W / 58.85334°N 98.63586°W |
Primary inflows | North Seal River (Ireland Lake) |
Primary outflows | North Seal River |
Basin countries | Canada |
Max. length | 26 km (16 mi) |
Max. width | 3.5 km (2.2 mi) |
Surface elevation | 250 m (820 ft) |
Settlements | None |
Stony Lake [1] is a lake in the northern Manitoba, Canada.
It is formed at an elevation of 250 m (820 ft), along the North Seal River, which flows east into the Seal River, which in turn empties into the Hudson Bay.
The community of Tadoule Lake, located 9 kilometers (5.6 mi) east of the southern arm of the lake, is the closest inhabited settlement.
Many islands raise from the lake, among them Moffatt Island, Seamen Island (largest), and Radcliffe Island.
Lake Winnipeg is a very large, relatively shallow 24,514-square-kilometre (9,465 sq mi) lake in North America, in the province of Manitoba, Canada. Its southern end is about 55 kilometres (34 mi) north of the city of Winnipeg. Lake Winnipeg is Canada's sixth-largest freshwater lake and the third-largest freshwater lake contained entirely within Canada, but it is relatively shallow excluding a narrow 36 m (118 ft) deep channel between the northern and southern basins. It is the eleventh-largest freshwater lake on Earth. The lake's east side has pristine boreal forests and rivers that were in 2018 inscribed as Pimachiowin Aki, a UNESCO World Heritage Site. The lake is 416 km (258 mi) from north to south, with remote sandy beaches, large limestone cliffs, and many bat caves in some areas. Manitoba Hydro uses the lake as one of the largest reservoirs in the world. There are many islands, most of them undeveloped.
The Assiniboine River is a 1,070-kilometre (660 mi) river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle, Souris, and Whitesand Rivers. For early history and exploration see Assiniboine River fur trade.
The Chipewyan are a Dene Indigenous Canadian people of the Athabaskan language family, whose ancestors are identified with the Taltheilei Shale archaeological tradition. They are part of the Northern Athabascan group of peoples, and hail from what is now Western Canada.
The Canadian Northern Railway (CNoR) was a historic Canadian transcontinental railway. At its 1923 merger into the Canadian National Railway, the CNoR owned a main line between Quebec City and Vancouver via Ottawa, Winnipeg, and Edmonton.
The Churchill River is a major river in Alberta, Saskatchewan and Manitoba, Canada. From the head of the Churchill Lake it is 1,609 kilometres (1,000 mi) long. It was named after John Churchill, 1st Duke of Marlborough and governor of the Hudson's Bay Company from 1685 to 1691. The Cree name for the river is Missinipi, meaning "big waters". The Denesuline name for the river is des nëdhë́, meaning "Great River".
The Boreal Shield Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is the largest ecozone in Canada. Covering 1.8 million square kilometres it covers almost 20% of Canada's landmass, stretching from northern Saskatchewan to Newfoundland.
Eastern Manitoba, or the Eastman Region, is an informal geographic region of the Canadian province of Manitoba. It is bounded on the north by the Winnipeg River and Lake Winnipeg, on the east by the Manitoba-Ontario border, on the south by the Canada–US border, and on the west by the Red River. With a population of 128,855 as of the 2021 Canadian census, the Eastman Region is the second most populous region outside of the Winnipeg Metropolitan Region.
Egenolf Lake is a lake in northern Manitoba, about 75 kilometres south of the provincial boundary with Nunavut, Canada. Pike have been caught at Egenolf Lake measuring well over 50 inches.
The history of post-confederation Canada began on July 1, 1867, when the British North American colonies of Canada, New Brunswick, and Nova Scotia were united to form a single Dominion within the British Empire. Upon Confederation, the United Province of Canada was immediately split into the provinces of Ontario and Quebec. The colonies of Prince Edward Island and British Columbia joined shortly after, and Canada acquired the vast expanse of the continent controlled by the Hudson's Bay Company, which was eventually divided into new territories and provinces. Canada evolved into a fully sovereign state by 1982.
The geography of Manitoba addresses the easternmost of the three prairie Canadian provinces, located in the longitudinal centre of Canada. Manitoba borders on Saskatchewan to the west, Ontario to the east, Nunavut to the north, and the American states of North Dakota and Minnesota to the south. Although the border with Saskatchewan appears straight on large-scale maps, it actually has many right-angle corners that give the appearance of a slanted line. In elevation, Manitoba ranges from sea level on Hudson Bay to 2727 ft (831 m) on top of Baldy Mountain. The northern sixty percent of the province is on the Canadian Shield. The northernmost regions of Manitoba lie permafrost, and a section of tundra bordering Hudson Bay.
Nueltin Lake straddles the Manitoba—Nunavut border in Canada. The lake, which has an area of 2,279 km2 (880 sq mi), is predominantly in Nunavut's Kivalliq Region, and on the Manitoba side there is the Nueltin Lake Airport which serves the fishing lodge. The lake is split into two parts by a set of narrows. It is drained by the Thlewiaza River.
The Stony Mountain Formation is a stratigraphical unit of Ashgill age in the Western Canadian Sedimentary Basin.
Knee Lake is part of the Hayes River in Manitoba, Canada. It was on the voyageurs route from York Factory on Hudson Bay to Norway House, Manitoba on Lake Winnipeg. It gets its name from a knee-like bend in the middle. The upstream western part is about 6 miles from south to north and less than 4 miles broad. The lake narrows to less than half a mile and then extends about 20 miles northeast, this section being at most 4 miles across. Near the knee is Magnetic Island with an ore body that is said to make compasses useless. Upstream from the lake, the Hayes River exits eastward out of Oxford Lake, goes over Trout Falls and widens into a long lake which joins Knee Lake at its southwest corner. The river exits the northeast end of the lake and after about 7 miles and four portages broadens into Swampy Lake. At the east end of Swampy Lake is the dramstone where west-bound voyageurs took a dram to celebrate leaving the most difficult part of the river.
Pipestone Creek is a river in the Souris River watershed. Its flow begins in southeastern Saskatchewan, just south of the town of Grenfell and travels in a southeastern direction into Manitoba in the Westman Region where it empties into Oak Lake through the Oak Lake Marsh.
Oak Lake is a lake in the south-western part of the Canadian province of Manitoba in a region called Westman. Oak Lake is a kettle lake and is an aquifer supplier for numerous nearby residential areas and farms. The lake is in the RM of Sifton and sits at an elevation of 426 metres above sea level. Provincial Road 254 provides access to the lake.
Plum Creek is the primary outflow for the Plum Lakes and travels in an easterly direction for about 28 kilometres until it meets up with the Souris River, which is part of the Hudson Bay drainage basin, at the community of Souris in the Canadian province of Manitoba. Plum Lakes and the beginning of Plum Creek are in the Rural Municipality of Sifton and the mouth is in the Municipality of Souris – Glenwood.
Sturgeon Bay Provincial Park is a provincial park on the western shore of Lake Winnipeg in Manitoba, Canada. The park is considered to be a Class Ib protected area under the IUCN protected area management categories. It is 144.9 km2 (55.9 sq mi) in size.