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Asessippi Provincial Park
Asessippi Provincial Park is a provincial park in the Rural Municipality of Riding Mountain West, Manitoba, Canada. It is located near Inglis, Manitoba, about west of Dauphin, and is in size. A campground on the south shore of the Shellmouth Reservoir has serviced and un-serviced sites as well as a group-use area. Asessippi Ski Resort is also in the area. The park is considered to be a Class III protected area under the IUCN protected area management categories, and was designated a provincial park by the Government of Manitoba on 9 April 1964. History Asessippi Park was established as part of the creation of the Shellmouth Dam and its reservoir, the Lake of the Prairies. The lake provides anglers with opportunities to fish for perch, northern pike, and walleye. ''Asessippi'' comes from the Cree language—the second part is the word ''sîpiy'' ('river'); and the first part may be the word ''êsa'' ('clam shell') or the word ''asinîs'' ('stone'). The park is named af ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inglis, Manitoba
Inglis is a local urban district in the Rural Municipality of Riding Mountain West, Manitoba, Canada. Located on Provincial Road 366. approximately east of Highway 83 between Russell and Roblin, Inglis is the closest community to the Asessippi Provincial Park, Asessippi Ski Area, and the Lake of the Prairies. Inglis is also the home of the Inglis Grain Elevators, a National Historic Site of Canada. History Inglis was established as a village on 1 January 1956. On May 1, the Inglis and District Credit Union Society received their Charter of Incorporation. The community was titled ''Inglis'' in the 1990s, named after Robert James Inglis a Scotsman from Montreal, Quebec, who supposedly tailored all of the uniforms for Canadian Pacific Railway. The name ''Inglis'' itself simply means 'English'. Notable people *Del Barber Delainey Doucha Barber (born October 14, 1983) is a Canadian independent folk, folk rock, Americana, and alternative country singer-songwriter, musici ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cree Language
Cree (also known as Cree– Montagnais–Naskapi) is a dialect continuum of Algonquian languages spoken by approximately 117,000 people across Canada, from the Northwest Territories to Alberta to Labrador. If considered one language, it is the aboriginal language with the highest number of speakers in Canada. The only region where Cree has any official status is in the Northwest Territories, alongside eight other aboriginal languages. There, Cree is spoken mainly in Fort Smith and Hay River. Names Endonyms are: * (Plains Cree) * (Woods Cree) * (Western Swampy Cree) * (Eastern Swampy Cree) * (Moose Cree) * (Southern East Cree) * (Northern East Cree) * (Atikamekw) * (Western Montagnais, Piyekwâkamî dialect) * (Western Montagnais, Betsiamites dialect) * (Eastern Montagnais) Origin and diffusion Cree is believed to have begun as a dialect of the Proto-Algonquian language spoken between 2,500 and 3,000 years ago in the original Algonquian homeland, an u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Agassiz
Lake Agassiz was a large glacial lake in central North America. Fed by glacial meltwater at the end of the last glacial period, its area was larger than all of the modern Great Lakes combined. First postulated in 1823 by William H. Keating, it was named by Warren Upham in 1879 after Louis Agassiz, when Upham recognized that the lake was formed by glacial action. Geological progression During the last ice age, northern North America was covered by an ice sheet, which alternately advanced and retreated with variations in the climate. This continental ice sheet formed during the period now known as the Wisconsin glaciation, and covered much of central North America between 30,000 and 10,000 years ago. As the ice sheet disintegrated, its meltwaters created an immense proglacial lake. Around 13,000 years ago, this lake came to cover much of what are now southeastern Manitoba, northwestern Ontario, northern Minnesota, eastern North Dakota, and Saskatchewan. At its greatest extent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meltwater Channel
A meltwater channel (or sometimes a glacial meltwater channel) is a channel cut into ice, bedrock or unconsolidated deposits by the flow of water derived from the melting of a glacier or ice-sheet. The channel may form on the surface of, within, beneath, along the margins of or downstream from the ice mass. Accordingly it would be referred to as supraglacial, englacial, subglacial, lateral (or ice-marginal) or proglacial. Different forms of subglacial channel are described in glaciological literature including Nye or N-channels, Röthlisberger or R-channels and Hooke or H-channels. Tunnel valley is a related term descriptive of subglacial channels. Some examples of tunnel valleys in northwest England have also been described as iceways. The depositional landforms known as kames and eskers may often be found in association with meltwater channels. An urstromtal is a proglacial or ice-marginal channel common in Germany and Poland formed during various of the Pleistocene glaciat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shell River (Assiniboine River)
The Shell River is a river in western Manitoba. It flows south from its source in Duck Mountain Provincial Park (Manitoba), Duck Mountain Provincial Park at the confluence of the East Shell River and West Shell River, to its mouth in Asessippi Provincial Park at the Shellmouth Reservoir, Lake of the Prairies where it joins the Assiniboine River. The river was originally a meltwater channel resulting from the melting of the Keewatin Ice Flow, part of Laurentide Ice Sheet more than ten thousand years ago. The modern day Shell River is much smaller and meanders within the large valley created by its glacier fed predecessor. It is an example of a misfit stream, where a river occupies a river channel that does not match its size. The river is bridged by: *Manitoba Provincial Road 367, PR 367 *Manitoba Provincial Road 594, PR 594 *Manitoba Provincial Road 584, PR 584 *Manitoba Provincial Road 591, PR 591 *Manitoba Highway 5, PTH 5 *Manitoba Provincial Road 583, PR 583 *Manitoba Highway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spillway
A spillway is a structure used to provide the controlled release of water downstream from a dam or levee, typically into the riverbed of the dammed river itself. In the United Kingdom, they may be known as overflow channels. Spillways ensure that water does not damage parts of the structure not designed to convey water. Spillways can include floodgates and fuse plugs to regulate water flow and reservoir level. Such features enable a spillway to regulate downstream flow—by releasing water in a controlled manner before the reservoir is full, operators can prevent an unacceptably large release later. Other uses of the term "spillway" include bypasses of dams and outlets of channels used during high water, and outlet channels carved through natural dams such as moraines. Water normally flows over a spillway only during flood periods, when the reservoir has reached its capacity and water continues entering faster than it can be released. In contrast, an intake tower is a structure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assiniboine River
The Assiniboine River (''; french: Rivière Assiniboine'') is a river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River of the North, Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle River, Qu'Appelle, Souris River, Souris and Whitesand River, Saskatchewan, Whitesand Rivers. For early history and exploration see Assiniboine River fur trade. The river takes its name from the Assiniboine people, Assiniboine First Nations in Canada, First Nation. Robert Douglas of the Geographical Board of Canada (1933) made several comments as to its origin: "The name commemorates the Assiniboine natives called by La Vérendrye in 1730 'Assiniboils' and by Governor Knight in 1715 of the Hudson's Bay Company 'stone Indians.' Assiniboine is the name of an Indian tribe and is deri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laurentide Ice Sheet
The Laurentide Ice Sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glacial epochs, from 2.58 million years ago to the present. The last advance covered most of northern North America between c. 95,000 and c. 20,000 years before the present day and, among other geomorphological effects, gouged out the five Great Lakes and the hosts of smaller lakes of the Canadian Shield. These lakes extend from the eastern Northwest Territories, through most of northern Canada, and the upper Midwestern United States (Minnesota, Wisconsin, and Michigan) to the Finger Lakes, through Lake Champlain and Lake George areas of New York, across the northern Appalachians into and through all of New England and Nova Scotia. At times, the ice sheet's southern margin included the present-day sites of coastal towns of the Northeastern United States, and cities such as Bos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Russell, Manitoba
Russell is an unincorporated urban community in the Municipality of Russell – Binscarth, Manitoba. It is located along PTH 16 and PTH 83, and is at the western terminus of PTH 45. Russell is approximately east of the Saskatchewan border and northwest of Winnipeg. The community is home to 1,611 people as of the 2011 census. The community was designated as a town prior to 1 January 2015, when it and the nearby Village of Binscarth amalgamated with the Rural Municipality of Russell. Russell is the home of Manitoba's Beef and Barley Festival, which is held annually in October to celebrate the region's strong agricultural tradition. Grain farming and cattle ranching are extensive in the surrounding areas. History European-Canadians first settled the area around Russell around 1880. The first post office began operations at a site north of the present community in 1880, and was called " Shell River". The closest Canadian Pacific Railway (CPR) point was renamed to ''Russell ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manitoba Highway 83
Provincial Trunk Highway 83 (PTH 83) is a major north-south highway that runs in the far western region of the Canadian province of Manitoba. It travels from the North Dakota border south of Melita, north through Virden, Birtle, Russell, and Roblin to its northern terminus with PTH 10 in the town of Swan River. Along with US 83, PTH 83 is part of the longest continuously numbered north-south highway in North America with a combined distance of . PTH 83 travels no further than east of the Saskatchewan border, and comes within of the provincial boundary from the junction with PR 487 just north of Benito to the junction with PTH 57. History PTH 83 first appeared on the 1953 Manitoba Highway Map. Prior to 1953, PTH 83 was originally numbered as '' Highway 22''. In 1953, the government re-designated it to match U.S. Route 83. As well, the current section of the highway between Russell and Swan River was known as ''Highway 31''. Originally, the highway's northern termin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sawmill
A sawmill (saw mill, saw-mill) or lumber mill is a facility where logs are cut into lumber. Modern sawmills use a motorized saw to cut logs lengthwise to make long pieces, and crosswise to length depending on standard or custom sizes (dimensional lumber). The "portable" sawmill is of simple operation. The log lies flat on a steel bed, and the motorized saw cuts the log horizontally along the length of the bed, by the operator manually pushing the saw. The most basic kind of sawmill consists of a chainsaw and a customized jig ("Alaskan sawmill"), with similar horizontal operation. Before the invention of the sawmill, boards were made in various manual ways, either rived (split) and planed, hewn, or more often hand sawn by two men with a whipsaw, one above and another in a saw pit below. The earliest known mechanical mill is the Hierapolis sawmill, a Roman water-powered stone mill at Hierapolis, Asia Minor dating back to the 3rd century AD. Other water-powered mills followe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flour Mill
A gristmill (also: grist mill, corn mill, flour mill, feed mill or feedmill) grinds cereal grain into flour and middlings. The term can refer to either the grinding mechanism or the building that holds it. Grist is grain that has been separated from its chaff in preparation for grinding. History Early history The Greek geographer Strabo reports in his ''Geography'' a water-powered grain-mill to have existed near the palace of king Mithradates VI Eupator at Cabira, Asia Minor, before 71 BC. The early mills had horizontal paddle wheels, an arrangement which later became known as the " Norse wheel", as many were found in Scandinavia. The paddle wheel was attached to a shaft which was, in turn, attached to the centre of the millstone called the "runner stone". The turning force produced by the water on the paddles was transferred directly to the runner stone, causing it to grind against a stationary "bed", a stone of a similar size and shape. This simple arrangement re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
