Wascana Creek
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Wascana Creek
Wascana Creek is a river in the Canadian province of Saskatchewan. It is a tributary of the Qu'Appelle River. Originating in the fields east of Regina near Vibank, Wascana Creek travels south-east for approximately before turning back west at Tyvan. The creek then travels in a north-westwardly direction following Highway 33 through Regina, where it was dammed by the Canadian Pacific Railway to create Wascana Lake. The lake was created to supply water for steam locomotives and to create a decorative image in Regina. Below the lake, the creek leaves Regina and ends at the Qu'Appelle River about 1 mile west of Lumsden. Sherwood Forest Bridge and Albert Memorial Bridge are two of the bridges that cross Wascana Creek. Near the mouth of the river in the Wascana Valley, is a provincial recreation site called Wascana Trails that were developed for use in the 2005 Canada Summer Games. A 2011 study by Environment Canada found the creek to have high levels of pollution. Wa ...
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Albert Memorial Bridge (Regina, Saskatchewan)
The Albert Memorial Bridge is a beam bridge that spans across the north and south banks of Wascana Creek along Albert Street in Regina, Saskatchewan. This functional war memorial is 256 metres (840 feet) long and 22 metres (72 feet) wide. History The Albert Memorial Bridge's construction was part of a larger relief project during the Great Depression, which also included draining and dredging the adjacent Wascana Lake, and building two islands in the lake. The bridge was designed by the architectural firm of Puntin, O'Leary and Coxall, as well as noted consulting engineer Claude A.P. Turner. The bridge is highly ornamented with Egyptian motifs, lamp standards, multiple flag-staffs, glazed terra-cotta balusters and buffalo heads. Although the bridge's cost was estimated at less than $100,000 before construction, the final cost was $250,000. It was ridiculed by the locals because of its cost and became known as "Bryant's Folly", after then- public works minister ...
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Environment And Climate Change Canada
Environment and Climate Change Canada (ECCC; french: Environnement et Changement climatique Canada),Environment and Climate Change Canada is the applied title under the Federal Identity Program; the legal title is Department of the Environment (). is the department of the Government of Canada responsible for coordinating environmental policies and programs, as well as preserving and enhancing the natural environment and renewable resources. It is also colloquially known by its former name, Environment Canada (EC; french: Environnement Canada, links=no). The minister of environment and climate change has been Steven Guilbeault since October 26, 2021; Environment and Climate Change Canada supports the minister's mandate to: "preserve and enhance the quality of the natural environment, including water, air, soil, flora and fauna; conserve Canada's renewable resources; conserve and protect Canada's water resources; forecast daily weather conditions and warnings, and provide detail ...
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Hudson Bay Drainage Basin
The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into Hudson Bay and adjoining waters. Spanning an area of about , the basin is almost totally in Canada (spanning parts of the Prairies, central and northern Canada), with a small portion in the United States (in Montana, the Dakotas, and Minnesota). The watershed's connection to the Labrador Sea is at the Hudson Strait's mouth between Resolution Island in the Qikiqtaaluk Region and Cape Chidley on the Labrador Peninsula. The watershed's headwaters to the south-west are on the Continental Divide of the Americas, bounded at Triple Divide Peak to the south, and Snow Dome to the north. The western and northern boundary of the watershed is the Arctic Divide, and the southern and eastern boundary is the Laurentian Divide. left, Rupert's Land, granted as a commercial monopoly to the Hudson's Bay Company in 1670 Hudson Bay is often considered part of the Arctic Ocean. For ex ...
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List Of Rivers Of Saskatchewan
This is a list of rivers of Saskatchewan, a province of Canada. The largest and most notable rivers are listed at the start, followed by rivers listed by drainage basin and then alphabetically. Principal river statistics ''SourcStatistics Canada' Rivers by drainage basin *Arctic Ocean watershed ** Fond du Lac River ** Cree River ***Rapid River (Cree River tributary) ** Geikie River (Wollaston Lake) ** Clearwater River ***Graham Creek (Alberta) **Firebag River *Hudson Bay drainage basin **Assiniboine River ***Qu'Appelle River ****Moose Jaw River *****Avonlea Creek *****Thunder Creek **** Last Mountain Creek ***** Arm River *****Lanigan Creek ****Pheasant Creek ****Wascana Creek *** Whitesand River **** Spirit Creek ****Yorkton Creek ***** Crescent Creek ***Souris River **** Graham Creek ****Antler River ****Des Lacs River **** Gainsborough Creek ****Moose Mountain Creek **** Long Creek ****Pipestone Creek ** Churchill River *** Beaver River ****Doré ...
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Fathead Minnow
Fathead minnow (''Pimephales promelas''), also known as fathead or tuffy, is a species of temperate freshwater fish belonging to the genus ''Pimephales'' of the cyprinid family. The natural geographic range extends throughout much of North America, from central Canada south along the Rockies to Texas, and east to Virginia and the Northeastern United States.Page, Lawrence M. and Brooks M. Burr (1991), ''Freshwater Fishes'', p. 129-130, Houghton Mifflin, New York, NY. This minnow has also been introduced to many other areas via bait bucket releases. Its golden, or xanthic, strain, known as the rosy-red minnow, is a very common feeder fish sold in the United States and Canada. This fish is best known for producing Schreckstoff (a distress signal). Physical description The fathead minnow in its wild form is generally dull olive-grey in appearance, with a dusky stripe extending along the back and side, and a lighter belly. There is a dusky blotch midway on the dorsal fin. Breeding ...
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Brook Stickleback
} The brook stickleback (''Culaea inconstans'') is a small freshwater fish that is distributed across the US and Canada. It grows to a length of about 2 inches. It occupies the northern part of the eastern United States, as well as the southern half of Canada. Small populations are scattered throughout the Mississippi-Great Lakes basin extending to Colorado, New Mexico, Kentucky, Tennessee, etc., though some of these areas are not native to the species. This small fish inhabits clear, cool streams and lakes. They eat small invertebrates, algae, insect larvae, and occasionally their own eggs. They are also preyed upon by smallmouth bass and northern pike. Feeding time is usually dawn and sunset. The brook stickleback does have active competition mostly from minnows, but feeding times are different, along with diet.Stewart, D.B. 2007.''Fish diets and food webs in the Northwest Territories: brook stickleback (''Culaea inconstans''). Canadian Manuscript Report of Fisheries and A ...
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Craven, Saskatchewan
Craven ( 2016 population: ) is a village in the Canadian province of Saskatchewan within the Rural Municipality of Longlaketon No. 219 and Census Division No. 6. The village lies north-east of the town of Lumsden in the Qu'Appelle Valley. It sits at the confluence of the Qu'Appelle River and Last Mountain Creek. The Craven Dam is on the east side of the village. Craven is host to an annual country music festival called Country Thunder Saskatchewan. Originally called the Big Valley Jamboree, it was first established by Father Lucien Larré as a fundraiser for his Bosco Homes for emotionally disturbed youth. A successor event, the Kinsmen Rock'N the Valley rock music festival, ran until 2004. The country music format was revived in 2005. History Craven was founded in 1882 by Colonel Stone and was originally called Sussex. The original settlement was located a half a mile east from the present site. Craven incorporated as a village on April 11, 1905. Demographics In ...
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Craven Dam
Craven Dam is at the confluence of the Qu'Appelle River and Last Mountain Creek and immediately east of the village of Craven on the Qu'Appelle River at SW 24-20-21 W2. It is in the Canadian province of Saskatchewan in the RM of Longlaketon No. 219. The dam does not create a reservoir as its purpose is to regulate water flow along the Qu'Appelle River. The dam is operated by the Saskatchewan Water Security Agency and can be accessed on the north side by Highway 99. Craven Dam is the dividing point between the upper and lower watersheds of the Qu'Appelle River. The total drainage basin of the Qu'Appelle River upstream from the dam is and it is divided into five sub-basins, which include Lanigan-Manitou, Wascana Creek, Last Mountain Lake, Upper Qu'Appelle, and Moose Jaw River. The original Craven Dam was built in 1943 and did not include a fishway. Starting in August of 2002 and finishing in 2003, Agriculture and Agri-Food Canada rebuilt the dam. The new dam included a ...
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Lanigan Creek
Lanigan Creek is a river in the Canadian province of Saskatchewan. It is located in the south central part of the province 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. The river starts north-west of the Quill Lakes, near the village of St. Gregor and the intersections of Highway 5 and Highway 667. It travels in a south-south-westwardly direction past the town of Lanigan and into the northern end of Last Mountain Lake. The river is part of the Upper Qu'Appelle River watershed, as Last Mountain Creek drains Last Mountain Lake into the Qu'Appelle River. The most northerly part of the Lanigan Creek Watershed also happens to be the most northerly point of the Red River Watershed. At the southern end of Lanigan Creek, at the point it empties into Last Mountain Lake, there's Last Mountain Lake Bird Sanctuary, which ...
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Last Mountain Lake
Last Mountain Lake, also known as Long Lake, is a prairie lake formed from glaciation 11,000 years ago. It is located in south central Saskatchewan, Canada, about north-west of the city of Regina. It flows into the Qu'Appelle River via Last Mountain Creek, which flows past Craven. It is approximately long, and wide at its widest point. It is the largest naturally occurring body of water in southern Saskatchewan. Only Lake Diefenbaker, which is man-made, is larger. The lake is a popular resort area for residents of south-eastern Saskatchewan. History In the late 1800s, access to the area for farming and settlement was opened up by the Qu'Appelle, Long Lake and Saskatchewan Railroad and Steamboat Company which also operated steamships on the lake. Until 1974, the lake was known as ''Long Lake''. It was renamed ''Last Mountain Lake'' in honour of a Plains Cree legend about the Great Spirit shovelling dirt from the valley the lake now occupies and forming Last Mount ...
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Moose Jaw River
Moose Jaw River is a river in the Canadian province of Saskatchewan. It is located in the southern part of the province 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. The Moose Jaw River drainage basin is one of five sub-basins that make up the Upper Qu'Appelle Watershed. Craven Dam at the village of Craven is the dividing point between the upper and lower watersheds of the Qu'Appelle River. The river and its tributaries drain a total of . The total combined drainage area for the five sub-basins of the Upper Qu'Appelle Watershed is . The Qu'Appelle River system is part of the much larger Hudson Bay drainage basin. Course The source of the Moose Jaw River is Ibsen Lake, which is about west of Yellow Grass. From there, the river travels in a north-westerly direction following Highway 39 most of the way to the cit ...
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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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