Niyanun Lake
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Niyanun Lake
Niyanun Lake is a glacial lake on the Mistik Creek chain in the Hudson Bay drainage basin in the Northern Region, Manitoba, Northern Region of Manitoba, Canada. It sits in the Churchill River Upland portion of the Midwestern Canadian Shield forests which consist of mixed deciduous and coniferous trees. The lake is also situated on the well known "Mistik Creek Loop", a remote canoe route in length which can be paddled in four days. ''Niyanun'' means 'five' in Cree, as all of the fourteen lakes on Mistik Creek are named in numeric order in Cree. The lake contains northern pike. The region around the lake consists of rocky parallel ridges with poorly drained areas of muskeg and irregular stony shorelines due to intense glaciation. See also *List of lakes of Manitoba References

{{authority control Lakes of Northern Manitoba Glacial lakes of Manitoba ...
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Manitoba
Manitoba ( ) is a Provinces and territories of Canada, province of Canada at the Centre of Canada, longitudinal centre of the country. It is Canada's Population of Canada by province and territory, fifth-most populous province, with a population of 1,342,153 as of 2021, of widely varied landscape, from arctic tundra and the Hudson Bay coastline in the Northern Region, Manitoba, north to dense Boreal forest of Canada, boreal forest, large freshwater List of lakes of Manitoba, lakes, and prairie grassland in the central and Southern Manitoba, southern regions. Indigenous peoples in Canada, Indigenous peoples have inhabited what is now Manitoba for thousands of years. In the early 17th century, British and French North American fur trade, fur traders began arriving in the area and establishing settlements. The Kingdom of England secured control of the region in 1673 and created a territory named Rupert's Land, which was placed under the administration of the Hudson's Bay Company. Rupe ...
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Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ...
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Mistik Creek
The Mistik Creek is a stream in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada, approximately northeast of Bakers Narrows. ''Mistik'' is a Cree word for 'Tree'. Description The remote creek flows through Churchill River Upland portion of the Midwestern Canadian Shield forests and is surrounded by mixed forest with stands of black spruce, white spruce, jack pine, and trembling aspen. The shoreline is characterized by steeply sloping irregular rock ridges and poorly drained areas of muskeg. Mistik Creek area is largely pristine and home to moose, black bear, lynx, wolf, and beaver. It is part of the range of the Naosap woodland caribou herd. Bird species include raven, common loon, spruce grouse, bald eagle and hawk owl. The creek is not easily accessible, but there is some trapping, hunting, and recreational fishing activity. Lakes Mistik Creek notably includes fourteen lakes, named in numeric order in Cree. In order from south to north, t ...
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Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ...
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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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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Northern Region, Manitoba
Northern Manitoba (also known as NorMan or Nor-Man) is a geographic and cultural region of the Canadian province of Manitoba. Originally encompassing a small square around the Red River Colony, the province was extended north to the 60th parallel in 1912. The region's specific boundaries vary, as "northern" communities are considered to share certain social and geographic characteristics, regardless of latitude. Geography Different bodies of the Government of Manitoba provide different definitions of Northern Manitoba. The most detailed description is set out by Manitoba Indigenous and Northern Relations: For marketing purposes, Travel Manitoba considers Northern Manitoba to encompass everything north of the 53rd parallel. In contrast, the Look North economic development agency defines the North as consisting of Statistics Canada's Census Divisions 19, 21, 22, and 23. There is also a defined territory of responsibility for the Northern Regional Health Authority, which exclud ...
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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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Midwestern Canadian Shield Forests
The Midwestern Canadian Shield forests ecoregion, in the Taiga and Boreal forests Biome, are of northern Canada. Setting This is an area of rolling hills with lakes both small and large, wetlands, and rocky outcrops on the Canadian Shield in northern Saskatchewan, north-central Manitoba (north and east of Lake Winnipeg) and Northwestern Ontario. Specific areas include the Athabasca Sand Dunes, and many lakes such as Cree Lake, Upper Foster Lake and Reindeer Lake in Saskatchewan. The area has a cold climate, very cold in winter although the hills around Lac Seul are warmer and wetter than most of the ecoregion, while the Athabasca Plain and the uplands above the Churchill River and Hayes River are cooler. There are patches of permafrost throughout Flora Much of the landscape, including the Athabasca Plain, is the boreal forest that covers so much of Canada at this latitude, consisting of black spruce (''Picea mariana''), jack pine (''Pinus banksiana''), quaking aspen (''Populu ...
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Cree
The Cree ( cr, néhinaw, script=Latn, , etc.; french: link=no, Cri) are a Indigenous peoples of the Americas, North American Indigenous people. They live primarily in Canada, where they form one of the country's largest First Nations in Canada, First Nations. In Canada, over 350,000 people are Cree or have Cree ancestry. The major proportion of Cree in Canada live north and west of Lake Superior, in Ontario, Manitoba, Saskatchewan, Alberta and the Northwest Territories. About 27,000 live in Quebec. In the United States, Cree people historically lived from Lake Superior westward. Today, they live mostly in Montana, where they share the Rocky Boy Indian Reservation with Ojibwe (Chippewa) people. The documented westward migration over time has been strongly associated with their roles as traders and hunters in the North American fur trade. Sub-groups / Geography The Cree are generally divided into eight groups based on dialect and region. These divisions do not necessarily r ...
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Northern Pike
The northern pike (''Esox lucius'') is a species of carnivorous fish of the genus '' Esox'' (the pikes). They are typical of brackish and fresh waters of the Northern Hemisphere (''i.e.'' holarctic in distribution). They are known simply as a pike in Britain, Ireland, and most of Eastern Europe, Canada and the United States. Pike can grow to a relatively large size: the average length is about , with maximum recorded lengths of up to and published weights of . The IGFA currently recognizes a pike caught by Lothar Louis on Greffern Lake, Germany, on 16 October 1986, as the all-tackle world-record northern pike. Northern pike grow to larger sizes in Eurasia than in North America, and typically grow to larger sizes in coastal than inland regions of Eurasia. Etymology The northern pike gets its common name from its resemblance to the pole-weapon known as the pike (from the Middle English for 'pointed'). Various other unofficial trivial names are common pike, Lakes pike, great n ...
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Muskeg
Muskeg (Ojibwe: mashkiig; cr, maskīk; french: fondrière de mousse, lit. ''moss bog'') is a peat-forming ecosystem found in several northern climates, most commonly in Arctic and boreal areas. Muskeg is approximately synonymous with bog or peatland, and is a standard term in Western Canada and Alaska. The term became common in these areas because it is of Cree origin; (ᒪᐢᑫᐠ) meaning low-lying marsh. Muskeg consists of non-living organic material in various states of decomposition (as peat), ranging from fairly intact sphagnum moss, to sedge peat, to highly decomposed humus. Pieces of wood can make up five to fifteen percent of the peat soil. The water table tends to be near the surface. The sphagnum moss forming it can hold fifteen to thirty times its own weight in water, which allows the spongy wet muskeg to also form on sloping ground. Muskeg patches are ideal habitats for beavers, pitcher plants, agaric mushrooms and a variety of other organisms. Composit ...
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