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Mistusinne, Saskatchewan
Mistusinne ( 2016 population: ) is a resort village in the Canadian province of Saskatchewan within Census Division No. 7. It is on the shores of Gordon McKenzie Arm of the South Saskatchewan River in the Rural Municipality of Maple Bush No. 224. History The resort village's name is derived from the Plains Cree word ''mistasiniy'' or ''mistaseni'' (meaning "big stone"), which refers to a 400-ton glacial erratic that resembled a sleeping bison. It once rested in the Qu'Appelle Valley and served as a sacred gathering place for the Cree and Assiniboine peoples. before Lake Diefenbaker was built. During the South Saskatchewan River dam project, the erratic was in the flood path of the new reservoir that would become Lake Diefenbaker. In 1966, the Prairie Farm Rehabilitation Administration had the rock blasted apart with explosives, despite efforts by groups to save it. Pieces of the rock were used in monuments to Chief Poundmaker and a memorial to the boulder itself in Elbow. La ...
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List Of Resort Villages In Saskatchewan
A resort village is a type of incorporated urban municipality in the Canadian province of Saskatchewan. A resort village is created from an organized hamlet by the Minister of Municipal Affairs by ministerial order via section 51 of ''The Municipalities Act'' if the community has: *been an organized hamlet for three or more years; *a population of 100 or more; *50 or more dwellings or businesses; and *a taxable assessment base that meets a prescribed minimum. Saskatchewan has 40 resort villages that had a cumulative population of 4,118 and an average population of 103 in the 2011 Census. Saskatchewan's largest and smallest resort villages are Candle Lake and the Lumsden Beach with populations of 765 and 10 respectively. A resort village council may request the Minister of Municipal Affairs to change its status to a town if the resort village has a population of 500 or more. __FORCETOC__ List Gallery File:Cochin Lighthouse 2 (9195672467).jpg, Lighthouse atop Piro ...
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List Of Saskatchewan Provincial Highways
This is a list of Saskatchewan's highways: Only Highways 1, 2, 5, 6, 7, 11, 12, 16, and 39 contain sections of divided highway. Speed limits range from 90 km/h (55 mph) to 110 km/h (70 mph). Saskatchewan is the only province bordering the United States with no direct connection to the Interstate Highway System. Named routes * Can Am Highway * Circle Drive *Hanson Lake Road * Little Swan Road * Louis Riel Trail * McBride Lake Road * Northern Woods and Water Route * Ring Road * Red Coat Trail * Regina Bypass *Saskatoon Freeway * Saskota Travel Route * Trans-Canada Highway *Veterans Memorial Highway * Yellowhead Highway Primary (1–99) These are primary highways maintained by the provincial government. Almost all of these highways are paved for most of their length. Highways 1, 11, and 16 are the most important highways and are divided highways for much of their lengths, with some sections at expressway or freeway standards. ...
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Prairie Farm Rehabilitation Administration
The Prairie Farm Rehabilitation Administration (PFRA) was a branch under Agriculture and Agri-Food Canada (AAFC), a department of the Federal Government of Canada. The Prairie Farm Rehabilitation Administration was established by an Act of Parliament under Prime Minister R. B. Bennett in 1935 in response to the widespread drought, farm abandonment and land degradation of the 1930s. Its mandate was to: "... secure the rehabilitation of the drought and soil drifting areas in the Provinces of Manitoba, Saskatchewan and Alberta, and to develop and promote within those areas, systems of farm practice, tree culture, water supply, land utilization and land settlement that will afford greater economic security..." With this mandate, the PFRA served to promote sustainable development on the rural prairies for over seven decades in the areas of air, water, soils, and biodiversity. Its mandate included detailed examination of various methods for soil conservation and enrichment. The PFRA t ...
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Lake Diefenbaker
Lake Diefenbaker is a reservoir and bifurcation lake in Southern Saskatchewan, Canada. It was formed by the construction of Gardiner Dam and the Qu'Appelle River Dam across the South Saskatchewan and Qu'Appelle Rivers respectively. Construction began in 1959 and the lake was filled in 1967. The lake is long with approximately of shoreline. It has a maximum depth of , while the water levels regularly fluctuate 3–9 metres (9–27 feet) each year. Lake Diefenbaker provides water for domestic irrigation and town water supplies. The flow of the two rivers is now regulated with a considerable portion of the South Saskatchewan diverted into the Qu'Appelle. Prior to the dams' construction, high water levels in the South Saskatchewan would frequently cause dangerous ice conditions downstream in Saskatoon while the Qu'Appelle would frequently dry up in the summer months. Lake Diefenbaker is the largest body of water in southern Saskatchewan, although Last Mountain Lake is th ...
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Assiniboine
The Assiniboine or Assiniboin people ( when singular, Assiniboines / Assiniboins when plural; Ojibwe: ''Asiniibwaan'', "stone Sioux"; also in plural Assiniboine or Assiniboin), also known as the Hohe and known by the endonym Nakota (or Nakoda or Nakona), are a First Nations/Native American people originally from the Northern Great Plains of North America. Today, they are centred in present-day Saskatchewan. They have also populated parts of Alberta and southwestern Manitoba in Canada, and northern Montana and western North Dakota in the United States. They were well known throughout much of the late 18th and early 19th century, and were members of the Iron Confederacy with the Cree. Images of Assiniboine people were painted by 19th-century artists such as Karl Bodmer and George Catlin. Names The Europeans and Americans adopted names that other tribes used for the Assiniboine; they did not until later learn the tribe's autonym, their name for themselves. In Siouan, they ...
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Qu'Appelle Valley
The Qu'Appelle River is a river in the Canadian provinces of Saskatchewan and Manitoba that flows east from Lake Diefenbaker in south-western Saskatchewan to join the Assiniboine River in Manitoba, just south of Lake of the Prairies, near the village of St. Lazare. It is located in a region called the Prairie Pothole Region of North America, which extends throughout three Canadian provinces and five U.S. states. It is also within Palliser's Triangle and the Great Plains ecoregion. With the construction of the Qu'Appelle River Dam and Gardiner Dam upstream, water flow was significantly increased and regulated. Most of the Qu'Appelle's present flow is actually water diverted from the South Saskatchewan River. Upper and lower watersheds According to the Saskatchewan Water Security Agency, the Qu'Appelle Valley is made up of two watersheds with the dividing point being Craven Dam on the east side of Craven: Lower Qu'Appelle Watershed The Lower Qu'Appelle Valley is loca ...
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Bison
Bison are large bovines in the genus ''Bison'' (Greek: "wild ox" (bison)) within the tribe Bovini. Two extant and numerous extinct species are recognised. Of the two surviving species, the American bison, ''B. bison'', found only in North America, is the more numerous. Although colloquially referred to as a buffalo in the United States and Canada, it is only distantly related to the true buffalo. The North American species is composed of two subspecies, the Plains bison, ''B. b. bison'', and the wood bison, ''B. b. athabascae'', which is the namesake of Wood Buffalo National Park in Canada. A third subspecies, the eastern bison (''B. b. pennsylvanicus'') is no longer considered a valid taxon, being a junior synonym of ''B. b. bison''. References to "woods bison" or "wood bison" from the eastern United States refer to this subspecies, not ''B. b. athabascae'', which was not found in the region. The European bison, ''B. bonasus'', or wisent, or zubr, or colloquially Euro ...
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Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Err ...
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Plains Cree Language
Plains Cree (endonym: ) is a dialect of the Algonquian language, Cree, which is the most populous Canadian indigenous language. Plains Cree is considered a dialect of the Cree-Montagnais language or a dialect of the Cree language that is distinct from the Montagnais language. Plains Cree is one of five main dialects of Cree in this second sense, along with Woods Cree, Swampy Cree, Moose Cree, and Atikamekw. Although no single dialect of Cree is favored over another, Plains Cree is the one that is the most widely used. Out of the 116,500 speakers of the Cree language, the Plains Cree dialect is spoken by about 34,000 people primarily in Saskatchewan and Alberta but also in Manitoba and Montana. The number of people who can speak an Aboriginal language, such as Plains Cree, has increased. For example, in the 2016 census, 263,840 people could speak an Aboriginal language well enough to conduct a conversation. From 1996 to 2016, the total number of people who were able to speak ...
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Resort Village
A resort village is a type of incorporated urban municipality in the Canadian province of Saskatchewan. A resort village is created from an organized hamlet by the Minister of Municipal Affairs by ministerial order via section 51 of ''The Municipalities Act'' if the community has: *been an organized hamlet for three or more years; *a population of 100 or more; *50 or more dwellings or businesses; and *a taxable assessment base that meets a prescribed minimum. Saskatchewan has 40 resort villages that had a cumulative population of 4,118 and an average population of 103 in the 2011 Census. Saskatchewan's largest and smallest resort villages are Candle Lake and the Lumsden Beach with populations of 765 and 10 respectively. A resort village council may request the Minister of Municipal Affairs to change its status to a town if the resort village has a population of 500 or more. __FORCETOC__ List Gallery File:Cochin Lighthouse 2 (9195672467).jpg, Lighthouse atop Piro ...
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Canada 2016 Census
The 2016 Canadian census was an enumeration of Canadian residents, which counted a population of 35,151,728, a change from its 2011 population of 33,476,688. The census, conducted by Statistics Canada, was Canada's seventh quinquennial census. The official census day was May 10, 2016. Census web access codes began arriving in the mail on May 2, 2016. The 2016 census marked the reinstatement of the mandatory long-form census, which had been dropped in favour of the voluntary National Household Survey for the 2011 census. With a response rate of 98.4%, this census is said to be the best one ever recorded since the 1666 census of New France. This census was succeeded by Canada's 2021 census. Planning Consultation with census data users, clients, stakeholders and other interested parties closed in November 2012. Qualitative content testing, which involved soliciting feedback regarding the questionnaire and tests responses to its questions, was scheduled for the fall of 2013, w ...
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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 conflu ...
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