Wood Mountain Hills
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Wood Mountain Hills
Wood Mountain Hills are a hilly plateau in the Canadian province of Saskatchewan. The hills are located in the southern part of the province and are part of the Missouri Coteau, which is part of the Laurentian Divide between the watersheds of the Hudson Bay drainage basin of the Arctic Ocean and the Gulf of Mexico of the Atlantic Ocean. The hills are in a semi-arid region known as Palliser's Triangle in the Great Plains ecoregion of North America. The Wood Mountain Hills are known locally as "the Bench" and, at a height of above sea level, are the second highest point of land in Western Canada east of the Rocky Mountains. The highest point is just to the west in the neighbouring Cypress Hills. Geography The south-eastern part of the Wood Mountain Hills was one of the few places in Canada that wasn't covered in ice during the Last Glacial Period. This preserved tertiary sands and gravels at higher the elevations while other parts of the hills have glacial drift and deep ...
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Missouri Coteau
The Missouri Coteau, or Missouri Plateau, (french: Coteau du Missouri) is a large plateau that stretches along the eastern side of the valley of the Missouri River in central North Dakota and north-central South Dakota in the United States. In the Canadian provinces of Saskatchewan and Alberta this physiographic region is classified as the Uplands Missouri Coteau, which is a part of the Great Plains Province or Alberta Plateau Region, which extends across the southwest corner of the province of Saskatchewan as well as the southeast corner of the province of Alberta. Historically, in Canada the area was known as the Palliser's Triangle and regarded as an extension of the Great American Desert and unsuitable for agriculture and thus designated by Canadian geographer and explorer John Palliser. The terrain of the Missouri Coteau features low hummocky, undulating, rolling hills, potholes, and grasslands. Apart from being a geographical area, the Missouri Coteau also has a cultural co ...
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Drift (geology)
In geology, drift is a name for all sediment (clay, silt, sand, gravel, boulders) transported by a glacier and deposited directly by or from the ice, or by glacial meltwater. Drift is often subdivided into (unsorted and) unstratified drift (glacial till) that forms moraines and stratified drift (glaciolacustrine and fluvioglacial sediments) that accumulates as stratified and sorted sediments in the form of outwash plains, eskers, kames, varves, and so forth. The term drift clay is a synonym for boulder clay. Both are archaic terms for glacial tills with a fine-grained matrix.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds., 2005. ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. In the United Kingdom, drift is also applied as a general term for all surficial, unconsolidated, rock debris and sediment that is moved from one place to accumulate in another and mapped separately or otherwise diffrerentiated from underlying ...
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Wheatgrass
Wheatgrass is the freshly sprouted first leaves of the common wheat plant (''Triticum aestivum''), used as a food, drink, or dietary supplement. Wheatgrass is served freeze dried or fresh, and so it differs from wheat malt, which is convectively dried. Wheatgrass is allowed to grow longer and taller than wheat malt. Like most plants, wheatgrass contains chlorophyll, amino acids, minerals, vitamins and enzymes. Claims about the health benefits of wheatgrass range from providing supplemental nutrition to having unique curative properties, but these claims have not been scientifically proven. Wheatgrass juice is often available at juice bars, and some people grow and juice their own in their homes. It is available fresh as produce, in tablets, frozen juice, and powder. Wheatgrass is also sold commercially as a spray, cream, gel, massage lotion, and liquid herbal supplement. Because it is extracted from wheatgrass sprouts (that is, before the wheat seed or "berry" begins to f ...
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Ecozones Of Canada
Canada has 20 major ecosystems -- ecozones, comprising 15 terrestrial units and 5 marine units. These ecozones are further subdivided into 53 ecoprovinces, 194 ecoregions, and 1,027 ecodistricts. These form the country's ecological land classification within the Ecological Land Classification framework adopted in 2017. They represent areas of the earth's surface representative of large and very generalized ecological units characterized by interactive and adjusting biotic and abiotic factors Terrestrial ecozones On November 20, 2017, Statistics Canada approved the Ecological Land Classification (ELC) framework as the official government standard in classifying the ecological regions of Canada. This framework mirrors that which was originally established in 1995, but revises number of ecodisiricts to 1,027 in order to better align them with the Soil Landscapes of Canada (SLC) database of Agriculture and Agri-Food Canada. Though this framework originally included 5 marine ecozon ...
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Prairies Ecozone
The Prairies Ecozone is a Canadian terrestrial ecozone which spans the southern areas of the Prairie provinces of Alberta, Saskatchewan, and Manitoba. It is a productive agricultural area, and is commonly referred to as "Canada's breadbasket". Farmland covers about 94% of the land, and is the dominant domestic economic activity of the zone, as well as an important factor in Canadian foreign trade. Natural gas and oil are abundant in the area. The corresponding Level II ecoregion of the US Environmental Protection Agency is the Great Plains Ecoregion. Geography Following Alberta's border with British Columbia, this ecozone is adjacent to the Montane Cordillera on the west. The two zones are bifurcated by the Boreal Plains about 70 kilometres southwest of Calgary, which also wraps around the remaining extent of the zone north of the United States border toward the Red River Valley. It is part of the Interior Plains, the Canadian extension of the Great Plains, and covers approx ...
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Poplar River (Montana–Saskatchewan)
The Poplar River is a tributary of the Missouri River, approximately long in Saskatchewan in Canada and Montana in the United States. It rises in several forks on the plains of southern Saskatchewan. The western fork rises near Killdeer, Saskatchewan and flows southeast, into northeastern Montana, past Richland and across Daniels County. The middle fork rises northwest of Rockglen, Saskatchewan and flows southeast, into northeastern Montana, and passes west of Scobey. The two forks unite in the northern Fort Peck Indian Reservation. The combined fork flows southeast, then south-southwest, and joins the Missouri River near Poplar. Along with the Milk River and Big Muddy Creek, it is one of three waterways in Canada that drain into the Gulf of Mexico. Variant names The Poplar River has also been known as: Lost Child Creek and Middle Fork Poplar River. See also *List of rivers of Saskatchewan *List of rivers of Montana The following is a partial list of rivers of ...
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Frenchman River
The Frenchman River, ( ats, níhʔɔɔtóóúníícááh, lit=white person river), also known locally as the Whitemud River, is a river in Saskatchewan, Canada and Montana, United States. It is a tributary of the Milk River, itself a tributary of the Missouri and in turn a part of the Mississippi River watershed that flows to the Gulf of Mexico. The river is approximately long. The name origin is uncertain, although both Métis and francophone settlers inhabited its banks at the turn of the 20th century. The Frenchman Formation, a stratigraphical unit of the Western Canadian Sedimentary Basin, was named for the river. Course The headwaters are found in Cypress Lake, in the Cypress Hills, at an elevation of . It flows east towards Eastend, then turns south-east. Various reservoirs are built on its course (Eastend Reservoir, Huff Lake, Newton Lake) and the river is used extensively for irrigation. The river becomes meandered as it flows through the Grasslands National Park. ...
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Milk River (Alberta–Montana)
The Milk River is a tributary of the Missouri River, long, in the U.S. state of Montana and the Canadian province of Alberta. Rising in the Rocky Mountains, the river drains a sparsely populated, semi-arid watershed of , ending just east of Fort Peck, Montana. Geography It is formed in Glacier County in northwestern Montana, north of Browning, Montana, by the confluence of its South and Middle forks. The long South Fork and long Middle Fork both rise in the Rocky Mountains just east of Glacier National Park, in the Blackfeet Indian Reservation. Much of the water in the North Fork is diverted from the St. Mary River through a canal and inverted siphon. The main stream flows east-northeast into southern Alberta, where it is joined by the North Fork of the Milk River, from there It flows past the town of Milk River and Writing-on-Stone Provincial Park, then turns southeast into Montana, running east along the north side of the Sweetgrass Hills, turning south, passing ...
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Wood River (Saskatchewan)
Wood River is a river in the Canadian province of Saskatchewan. It has its source in the Wood Mountain Hills of south-western Saskatchewan and flows in a north-easterly direction to its mouth at Old Wives Lake. Old Wives Lake is a salt water lake with no outflow. As a result, the drainage basin of Wood River is an endorheic one. Along the course of the river, there are several parks, historical sites, and small towns. Course and description Wood River begins in south-western Saskatchewan at the height of the Wood Mountain Hills in semi-arid grasslands within a large region called Palliser's Triangle. Much of the northern half of Wood Mountain Hills is in the Wood River watershed while the southern half flows south into the United States and the drainage basin of the Milk River – a tributary of the Missouri River. This part of the drainage divide is known as the Missouri Coteau. Beginning at Pinto Butte at over , Wood River flows eastward through grasslands, rolling hil ...
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Endorheic Basin
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔνδον ''éndon'' 'wit ...
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Old Wives Lake
Old Wives Lake is a shallow saline lake in south central Saskatchewan, Canada, about 30 km south-west of Moose Jaw. The lake is fed by the Wood River but seasonal water relatively flattened the terrain, and as such results in significant mudflats. A Migratory Bird Sanctuary was established at the lake on March 9, 1925. This lake, in conjunction with Reed Lake and Chaplin Lake, forms a site of hemispheric importance in the Western Hemisphere Shorebird Reserve Network. It was designated in April 1997, and is "one of the most important inland sites for migratory birds in North America". A variety of First Nations oral traditions explain the origin of the lake's name. At various times during the lake's human history, it has attracted interest from several First Nations tribes, duck hunters, military trainers, sodium sulfate producers, conservationists, and birdwatchers. A town of the same name ( Old Wives) is located north of the lake on Highway 363. Name According to a ...
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Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ...
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