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Saskatchewan River
The Saskatchewan River (Cree: ''kisiskāciwani-sīpiy'', "swift flowing river") is a major river in Canada. It stretches about from where it is formed by the joining together of the North Saskatchewan and South Saskatchewan Rivers to Lake Winnipeg. It flows roughly eastward across Saskatchewan and Manitoba to empty into Lake Winnipeg. Through its tributaries the North Saskatchewan and South Saskatchewan, its watershed encompasses much of the prairie regions of Canada, stretching westward to the Rocky Mountains in Alberta and north-western Montana in the United States. Including its tributaries, it reaches to its farthest headwaters on the Bow River, a tributary of the South Saskatchewan in Alberta. Description It is formed in central Saskatchewan, approximately east of Prince Albert, by the confluence of its two major branches, the North Saskatchewan and the South Saskatchewan, at the Saskatchewan River Forks. Both source rivers originate from glaciers in the Alberta Ro ...
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South Saskatchewan River
The South Saskatchewan River is a major river in Canada that flows through the provinces of Alberta and Saskatchewan. For the first half of the 20th century, the South Saskatchewan would completely freeze over during winter, creating spectacular ice breaks and dangerous conditions in Saskatoon, Medicine Hat and elsewhere. At least one bridge in Saskatoon was destroyed by ice carried by the river. The construction of the Gardiner Dam in the 1960s, however, lessened the power of the river by diverting a substantial portion of the South Saskatchewan's natural flow into the Qu'Appelle River. By the 1980s many permanent sandbars had formed due to the lowering of the level of the river. From the headwaters of the Bow River, the South Saskatchewan flows for . At its mouth at Saskatchewan River Forks, it has an average discharge of and has a watershed of , 1,800 of which are in Montana in the United States and in Alberta and Saskatchewan. Course The river originates at the confluence o ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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Saskatchewan River Forks
Saskatchewan River Forks refers to the area in Canada where the North Saskatchewan and South Saskatchewan rivers merge to create the Saskatchewan River. It is about east of Prince Albert, Saskatchewan. The province of Saskatchewan maintains the Saskatchewan Forks Recreation Site, on the west side of the fork, which is heavily wooded, and features steep banks, a tourist picnic site and hiking trails. North American fur trade posts were of importance to European traders. Englishman Henry Kelsey, working for the Hudson's Bay Company, reached this point in 1692 but did not establish a fort. A New France fur-trading post, Fort La Jonquière, was established on the Saskatchewan or its branches in 1751 by Jacques Legardeur de Saint-Pierre, possibly at or near the forks. In 1753 a second French fur-trading post, Fort de la Corne, was established in the area by Louis de la Corne, Chevalier de la Corne. A major intersection when waterways were important to transportation on the Canadian pra ...
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First Nations In Canada
First Nations (french: Premières Nations) is a term used to identify those Indigenous Canadian peoples who are neither Inuit nor Métis. Traditionally, First Nations in Canada were peoples who lived south of the tree line, and mainly south of the Arctic Circle. There are 634 recognized First Nations governments or bands across Canada. Roughly half are located in the provinces of Ontario and British Columbia. Under Charter jurisprudence, First Nations are a "designated group," along with women, visible minorities, and people with physical or mental disabilities. First Nations are not defined as a visible minority by the criteria of Statistics Canada. North American indigenous peoples have cultures spanning thousands of years. Some of their oral traditions accurately describe historical events, such as the Cascadia earthquake of 1700 and the 18th-century Tseax Cone eruption. Written records began with the arrival of European explorers and colonists during the Age of Dis ...
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Nelson River
The Nelson River is a river of north-central North America, in the Canadian province of Manitoba. The river drains Lake Winnipeg and runs before it ends in Hudson Bay. Its full length (including the Saskatchewan River and Bow River) is , it has mean discharge of , and has a drainage basin of , of which is in the United States. Geography The Nelson River flows into Playgreen Lake from Lake Winnipeg then flows from two channels into Cross Lake. The east channel and the Jack River flow from the southeast portion of the lake into Little Playgreen Lake then the Nelson east channel continues in a northerly direction passing through Pipestone Lake on its way to Cross Lake. The west channel flows out of the north ends of Playgreen Lake, Kiskittogisu Lake and Kiskitto Lake into Cross Lake at the Manitoba Hydro's Jenpeg Generating Station and Dam. From Cross Lake it flows through Sipiwesk Lake, Split Lake and Stephens Lake on its way to the Hudson Bay. Since it drains Lake Winni ...
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Hudson Bay
Hudson Bay ( crj, text=ᐐᓂᐯᒄ, translit=Wînipekw; crl, text=ᐐᓂᐹᒄ, translit=Wînipâkw; iu, text=ᑲᖏᖅᓱᐊᓗᒃ ᐃᓗᐊ, translit=Kangiqsualuk ilua or iu, text=ᑕᓯᐅᔭᕐᔪᐊᖅ, translit=Tasiujarjuaq; french: baie d'Hudson), sometimes called Hudson's Bay (usually historically), is a large body of saltwater in northeastern Canada with a surface area of . It is located north of Ontario, west of Quebec, northeast of Manitoba and southeast of Nunavut, but politically entirely part of Nunavut. Although not geographically apparent, it is for climatic reasons considered to be a marginal sea of the Arctic Ocean. It Hudson Bay drainage basin, drains a very large area, about , that includes parts of southeastern Nunavut, Alberta, Saskatchewan, Ontario, Quebec, all of Manitoba, and parts of the U.S. states of North Dakota, South Dakota, Minnesota, and Montana. Hudson Bay's southern arm is called James Bay. The Cree language, Eastern Cree name for Hudson an ...
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Cedar Lake (Manitoba)
Cedar Lake is a lake just north of Lake Winnipegosis in Manitoba, Canada. Cedar Lake's water level is controlled by the Grand Rapids dam. The town of Grand Rapids and the First Nations town of Easterville are nearby. The lake is known to have excellent examples of prehistoric amber fossil of cretaceous age. This type of amber is called as "Chemawinit", according to an Indian tribe which lives in this area. Another name of this amber is "Cedarit". This amber contains many organic inclusions. To date, these inclusions have not been thoroughly researched. The lake's main source is the Saskatchewan River, which forms a delta on the northwest side of the lake. The flow of the Saskatchewan River to Lake Winnipeg on the eastern end of Cedar Lake is regulated by the Grand Rapids dam built in 1962 by Manitoba Hydro. See also *Saskatchewan River Delta *List of lakes of Manitoba This is an incomplete list of lakes of Manitoba, a province of Canada. Larger lake statistics The total are ...
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River Delta
A river delta is a landform shaped like a triangle, created by deposition (geology), deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rarely) another river that cannot carry away the supplied sediment. It is so named because its triangle shape resembles the Greek letter Delta. The size and shape of a delta is controlled by the balance between watershed processes that supply sediment, and receiving basin processes that redistribute, sequester, and export that sediment. The size, geometry, and location of the receiving basin also plays an important role in delta evolution. River deltas are important in human civilization, as they are major agricultural production centers and population centers. They can provide Coast, coastline defense and can impact drinking water supply. They are also Ecology, ecologically important, with different species' assemblages ...
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Carrot River (Saskatchewan)
The Carrot River is a river in north-eastern Saskatchewan, and north-western Manitoba. Its headwaters originate in the Cudworth and Tiger Hill Plains near the Town of Wakaw. The outlet of Wakaw Lake marks the beginning of the Carrot River and, from there, this river flows northeast through the Melfort and Red Earth Plains until it joins into the Saskatchewan River west of The Pas, Manitoba. The Carrot River is about 300 km in length and it parallels the course of the South Saskatchewan and Saskatchewan Rivers. The Carrot River serves as the main watershed for north-eastern Saskatchewan as all smaller streams and rivers empty into the Carrot River. This causes major flood problems during the spring run off and rainy seasons around the Town of Carrot River and Red Earth Indian Reserve. The floods usually strand everyone east of the river with very few ways around the flooded area. Another Carrot River enters Oxford Lake on the Hayes River. History The Carrot River va ...
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Mossy River
Mossy River is a river in the Canadian province of Saskatchewan. The river's source is east of Little Bear Lake and north-east of Narrow Hills Provincial Park in a hilly plateau called Cub Hills. The river travels through hills, boreal forest, and muskeg for about 100 kilometres en route to its mouth in the Saskatchewan River Delta. Highway 920 is the only road to access the mainstem of the river and there are no communities nor settlements along the course of the river. Description Mossy River begins at a small lake in the Cub Hills, just east of Little Bear Lake. Over 10,000 years ago at the end of the last ice age, the retreating glaciers shaped the landforms of the Cub Hills forming the valleys, lakes, and streams. The Mossy River flows east out of the hills through a glacier formed valley and into flatter land characterised by muskeg and boreal forest. The river meets Highway 920 as it flows out of the hills and is then met by Scarth River. From the Cub Hills, the riv ...
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Torch River
Torch River is a river in the Canadian province of Saskatchewan. The river's source is the dam at Candle Lake, near Candle Lake Provincial Park, and it travels east through boreal forest and muskeg en route to its mouth in the Saskatchewan River Delta. Torch River Provincial Forest, a conservation area, is located along the course of the river, near where White Fox River flows into Torch River. Torch River is a significant tributary of the Saskatchewan River and it is part of the Hudson Bay drainage basin. Description The Torch River is a tributary of the Saskatchewan River and it flows into one of North America's largest inland fresh water deltas, the Saskatchewan River Delta. The river begins at the south-east corner of Candle Lake from a dam at Hanson Bay near Minowakaw Beach Campground in the RM of Paddockwood No. 520. The dam is a 3.1-metre high concrete dam that was constructed in 1978–1979 and is operated by the Saskatchewan Watershed Authority. Less than a mil ...
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Tobin Lake
Tobin Lake is a reservoir along the course of the Saskatchewan River in the Canadian province of Saskatchewan. Tobin Lake was formed by the building of the E.B. Campbell Dam on the Saskatchewan River in 1963. The dam was originally named ''Squaw Rapids Dam'', but was renamed E.B. Campbell Dam in 1988 as the term ''squaw'' is derogatory. The town of Nipawin is near the western end of the lake and upstream from Nipawin along the Saskatchewan River is Codette Lake, which was formed by the construction of the Francois Finlay Dam in 1986. Situated between these two man-made lakes, Nipawin earned the nickname ''The Town of Two Lakes''. Most of the lake is in the RMs of Moose Range No. 486 and Torch River No. 488; the northernmost shoreline is in the Northern Saskatchewan Administration District. Access to the west and north side of the lake is from Highway 35, the east side from Highway 123, and on the south-west corner from Highway 255. The resort community of Tobin Lake is ...
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