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Carmichael, Saskatchewan
Carmichael is a special service area within the Rural Municipality of Carmichael No. 109, Saskatchewan, Canada that held village status prior to 2019. The population was 58 at the 2016 Census. Carmichael lies south of Highway 1 commonly known as the Trans Canada Highway, approximately east of city of Medicine Hat, Alberta. History Carmichael incorporated as a village on May 25, 1917. It restructured on December 31, 2018, relinquishing its village status in favour of becoming a special service area under the jurisdiction of the Rural Municipality of Carmichael No. 109. Demographics Attractions * Big Muddy Badlands, a series of badlands in southern Saskatchewan and northern Montana along Big Muddy Creek (Missouri River tributary), Big Muddy Creek. They are found in the Big Muddy Valley, a cleft of erosion and sandstone along Big Muddy Creek. The valley is long, wide and deep. The valley was formed when it was part of an ancient glacial meltwater channel that carr ...
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Special Service Area
Communities in the Province of Saskatchewan, Canada include Incorporation (municipal government), incorporated municipalities, Unincorporated community, unincorporated communities and First Nations in Canada, First Nations communities. Types of incorporated municipalities include urban municipalities, List of rural municipalities in Saskatchewan, rural municipalities and northern municipalities. Urban municipalities are further classified into four sub-types – City, cities, towns, villages and resort villages. Northern municipalities, which are located in the Northern Saskatchewan Administration District (NSAD), are further classified into three sub-types – northern towns, northern villages and northern hamlets. Rural municipalities are not classified into sub-types. Types of unincorporated communities include Hamlet (place), hamlets and organized hamlets within rural municipalities and northern settlements within the NSAD. The administration of rural municipalities, towns, ...
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Saskatchewan Highway 1
Highway 1 is the Saskatchewan section of the Trans-Canada Highway mainland route. The total distance of the Trans-Canada Highway in Saskatchewan is . The highway traverses Saskatchewan from the western border with Alberta, from Highway 1, to the Manitoba border where it continues as PTH 1. The Trans-Canada Highway Act was passed on December 10, 1949. The Saskatchewan segment was completed August 21, 1957, and completely twinned on November 6, 2008. The speed limit along the majority of the route is 110 kilometres per hour (70 mph) with urban area thoroughfares slowing to a speed of 80–100 kilometres per hour (50–62 mph). Portions of the highway—the section through Swift Current, an section east of Moose Jaw, and a section between the West Regina Bypass and Balgonie—are controlled-access. Highway 1 serves as a major east-west transport route for commercial traffic. It is the main link between southern Saskatchewan's largest cit ...
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North-West Mounted Police
The North-West Mounted Police (NWMP) was a Canadian para-military police force, established in 1873, to maintain order in the new Canadian North-West Territories (NWT) following the 1870 transfer of Rupert’s Land and North-Western Territory to Canada from the Hudson’s Bay Company, the Red River Rebellion and in response to lawlessness, demonstrated by the subsequent Cypress Hills Massacre and fears of United States military intervention. The NWMP combined military, police and judicial functions along similar lines to the Royal Irish Constabulary. A small, mobile police force was chosen to reduce potential for tensions with the United States and First Nations in Canada, First Nations. The NWMP uniforms included red coats deliberately reminiscent of British and Canadian military uniforms. The NWMP was established by the Canadian government during the ministry of Prime Minister of Canada, Prime Minister Sir John A. Macdonald, John Macdonald who defined its purpose as "the pres ...
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List Of National Historic Sites Of Canada
National Historic Sites of Canada (french: Lieux historiques nationaux du Canada) are places that have been designated by the federal Minister of the Environment on the advice of the Historic Sites and Monuments Board of Canada (HSMBC), as being of national historic significance. Parks Canada, a federal agency, manages the National Historic Sites program. As of July 2021, there were 999 National Historic Sites, 172 of which are administered by Parks Canada; the remainder are administered or owned by other levels of government or private entities. The sites are located across all ten provinces and three territories, with two sites located in France (the Beaumont-Hamel Newfoundland Memorial and Canadian National Vimy Memorial). There are related federal designations for National Historic Events and National Historic Persons. Sites, Events and Persons are each typically marked by a federal plaque of the same style, but the markers do not indicate which designation a subject has b ...
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Fort Walsh
Fort Walsh is a National Historic Sites of Canada, National Historic Site of Canada that was a North-West Mounted Police (NWMP) fort and the site of the Cypress Hills Massacre. Administered by Parks Canada, it forms a constituent part of Cypress Hills Interprovincial Park. The fort was built in June 1875 and was named for its builder, inspector James Morrow Walsh. The fort was intended to curb the illegal whiskey trade, protect Canada's nearby border with the United States, and aid with native policy. These factors had been brought to public attention following the Cypress Hills Massacre of 1873 and resulted in Prime Minister John A. Macdonald's establishment of the NWMP. Assiniboine chiefs Man Who Takes the Coat, Long Lodge, and Lean Man signed adhesion to Treaty 4 at the fort on September 25, 1877. Fort Walsh served as the NWMP headquarters from 1878 to 1882. In 1883 the fort was closed and dismantled. The site of the fort was designated a National Historic Sites of Canada, ...
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Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ...
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Cypress Hills Interprovincial Park
Cypress Hills Interprovincial Park is a natural park in Canada straddling the Alberta / Saskatchewan boundary and jointly administered by the two provinces. Located south-east of Medicine Hat, it became Canada's first interprovincial park in 1989. The park consists of two protected areas, the west block, that straddles the Alberta / Saskatchewan boundary between Alberta Highway 41, the townsite of Elkwater, Saskatchewan Highway 615, Saskatchewan Highway 271, and Fort Walsh, and the centre block, an additional area of in Saskatchewan, west of Saskatchewan Highway 21. Geography The Cypress Hills plateau rises up to 200 metres above the surrounding prairie, to a maximum elevation of at "Head of the Mountain" at the west end in Alberta, making it Canada's highest point between the Canadian Rockies and the Labrador Peninsula. Eastward across the boundary is the highest point in Saskatchewan, at . The "West Block" of the Cypress Hills spans the provincial boundary. Battle ...
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Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ...
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Big Muddy Creek (Missouri River Tributary)
Big Muddy Creek is a tributary of the Missouri River, approximately 191 mi (307 km) long, in the Canadian province of Saskatchewan and the U.S. state of Montana. Its source is in the Big Muddy Badlands of Saskatchewan. Big Muddy Creek begins in southern Saskatchewan at Big Muddy Lake, east of Big Beaver, Saskatchewan. It flows south through the Big Muddy Badlands and into Sheridan County, Montana, past Redstone. From there, east past Plentywood and then south forming the eastern border of Fort Peck Indian Reservation. It joins the Missouri west of Culbertson. It was explored in 1805 by the Lewis and Clark Expedition, who called it Martha's River in their journals and noticed on their return voyage in 1806 that it had changed its mouth on the Missouri. Along with the Milk River and the Poplar River, it is one of three waterways in Canada that drain into the Gulf of Mexico. Variant names Big Muddy Creek has also been known as: Big Muddy River, Little Yellow Riv ...
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Montana
Montana () is a state in the Mountain West division of the Western United States. It is bordered by Idaho to the west, North Dakota and South Dakota to the east, Wyoming to the south, and the Canadian provinces of Alberta, British Columbia, and Saskatchewan to the north. It is the fourth-largest state by area, the eighth-least populous state, and the third-least densely populated state. Its state capital is Helena. The western half of Montana contains numerous mountain ranges, while the eastern half is characterized by western prairie terrain and badlands, with smaller mountain ranges found throughout the state. Montana has no official nickname but several unofficial ones, most notably "Big Sky Country", "The Treasure State", "Land of the Shining Mountains", and " The Last Best Place". The economy is primarily based on agriculture, including ranching and cereal grain farming. Other significant economic resources include oil, gas, coal, mining, and lumber. The health ca ...
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Badlands
Badlands are a type of dry terrain where softer sedimentary rocks and clay-rich soils have been extensively eroded."Badlands" in ''Chambers's Encyclopædia''. London: George Newnes, 1961, Vol. 2, p. 47. They are characterized by steep slopes, minimal vegetation, lack of a substantial regolith, and high drainage density.A.J. Parsons and A.D. Abrahams, Editors (2009) ''Geomorphology of Desert Environments'' (2nd ed.) Springer Science & Business Media Ravines, gullies, buttes, hoodoos and other such geologic forms are common in badlands. Badlands are found on every continent except Antarctica, being most common where there are unconsolidated sediments. They are often difficult to navigate by foot, and are unsuitable for agriculture. Most are a result of natural processes, but destruction of vegetation by overgrazing or pollution can produce anthropogenic badlands. Badlands topography Badlands are characterized by a distinctive badlands topography. This is terrain in which w ...
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Big Muddy Badlands
The Big Muddy Badlands are a series of badlands in southern Saskatchewan and northern Montana in the Big Muddy Valley and along Big Muddy Creek. Big Muddy Valley is a cleft of erosion and sandstone that is long, wide, and deep. Big Muddy Valley and Big Muddy Badlands were formed over 12,000 years ago near the end of the last ice age when a glacial lake outburst flood occurred from a pre-historic glacial lake located at present-day Old Wives Lake. Big Muddy Lake is a large salt lake at the heart of the badlands. Two other notable lakes, Willow Bunch Lake and Lake of the Rivers are farther upstream in the valley. A prominent feature of the badlands is Castle Butte (), which is an outcrop of sandstone and compressed clay that protrudes above the flat prairie. It has a height of and a circumference of . It is located south of Bengough on Highway 34, about halfway between Big Muddy Lake and Willow Bunch Lake. Ranching and tourism are important industries in the spar ...
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