The Qu'Appelle River is a river in the Canadian provinces of Saskatchewan and Manitoba that flows 430 kilometres (270 mi) 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 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 Grant Devine Dam, formerly Alameda Dam, is an embankment dam located in the Canadian province of Saskatchewan near Alameda and Oxbow. It was constructed in 1994 to control flows on Moose Mountain Creek and Souris River. It provides flood protection and irrigation for this area of Saskatchewan, along with protection for Minot, North Dakota. The Grant Devine Reservoir provides opportunities for recreational use such as boating and fishing. At the full supply level of 562 metres (1,844 ft), the reservoir holds 105,000,000 m3 (3.7×109 cu ft) of water. The project is owned and operated by the Saskatchewan Water Security Agency (formerly Saskatchewan Watershed Authority).
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 40 kilometres (25 mi) 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 93 km (58 mi) long, and 3 km (1.9 mi) across 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.
Gooseberry Lake is a lake in the Canadian province of Saskatchewan. It is a shallow, natural lake located north-west of Moose Mountain Lake in the Moose Mountain Creek watershed. The lake has a large catchment area and flows into Moose Mountain Lake via the east flowing Gooseberry Creek. It is in the Prairies Ecozone of Palliser's Triangle and the area around the lake has a knob and kettle landscape with poor drainage that, during years with heavy spring run-off or rains, is known to flood.
Buffalo Pound Lake is a eutrophic prairie lake in Saskatchewan, Canada, formed from glaciation about 10,000 years ago, on the Qu'Appelle River approximately 28 kilometres (17 mi) north of Moose Jaw and 11 kilometres (6.8 mi) north-east of Tuxford. The lake gets its name from the method used by First Nations people to capture the bison using the natural topography as corrals or buffalo pounds. Bison, once numbering more than 60 million on the prairies but almost extinct by 1900, were reintroduced into the area in 1972.
The Saskatchewan Water Security Agency is an arm's length organization responsible for the management of water resources to ensure safe drinking water sources and reliable water supplies for economic, environmental, and social benefits in Saskatchewan, Canada. The Agency is a Treasury Board Crown Corporation administered by a board of directors appointed by the provincial government. Water Security Agency is located in Moose Jaw, SK, Canada and is part of the Water, Sewage and Other Systems Industry. Water Security Agency has 320.5 full time equivalent employees across all of its locations.
McDonald Lake, also known as Rafferty Reservoir, is a reservoir in the south-eastern part of the Canadian province of Saskatchewan. It was created when the Rafferty Dam was built on the Souris River in 1994. Before the dam was built that flooded the Souris Valley, McDonald Lake was a small lake and marsh on the valley floor adjacent to the Souris River.
Moose Mountain Upland, Moose Mountain Uplands, or commonly Moose Mountain, is a hilly plateau located in the south-east corner of the Canadian province of Saskatchewan, that covers an area of about 13,000 square kilometres (5,000 sq mi). The upland rises about 200 metres (660 ft) above the broad, flat prairie which is about 600 metres (2,000 ft) above sea level. The highest peak is "Moose Mountain" at 830 metres (2,720 ft) above sea level. The upland was named Moose Mountain because of the large number of moose that lived in the area. When it was originally used by fur traders, Métis, and the Indigenous peoples, the plateau was called Montagne a la Bosse, which is French for "The Mountain of the Bump or Knob".
Pipestone Creek is a river in the Souris River watershed. Its flow begins in southeastern Saskatchewan, just south of the town of Grenfell and travels in a southeastern direction into Manitoba in the Westman Region where it empties into Oak Lake through the Oak Lake Marsh.
Moose Mountain Creek is a river in the Canadian province of Saskatchewan. Its source is the Chapleau Lakes near Montmartre and it is a tributary of the Souris River, which, in turn, is a tributary of the Assiniboine River. The whole system is part of the Red River watershed, which is part of the Hudson Bay drainage basin and 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.
Last Mountain Creek is a river in south-central Saskatchewan. It is a tributary of the Qu'Appelle River 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.
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.
Avonlea Creek is a river in the southern part of the Canadian province of Saskatchewan. It is 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. Avonlea Creek is a main tributary of the Moose Jaw River, which is part of the Upper Qu'Appelle Watershed and the Hudson Bay drainage basin.
Thunder Creek is a river in the Canadian province of Saskatchewan. The watershed of Thunder Creek is within the semi-arid Palliser's Triangle in south-central Saskatchewan. It begins at small, man-made reservoir near Lake Diefenbaker and flows in a south-easterly direction towards the city of Moose Jaw and the Moose Jaw River. The Moose Jaw River is a major tributary of the Qu'Appelle River For most of its course, Thunder Creek follows a valley called the Thunder Creek meltwater channel that was formed over 10,000 years ago near the end of the last ice age.
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 LSD 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.
Cowan River is a river in the west-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. The river begins at Cowan Lake Dam near the northern end of Cowan Lake and flows north-west through muskeg and forest to meet Beaver River. Beaver River then flows into Lac Île-à-la-Crosse and the Churchill River. The entirety of Cowen River is within the Northern Saskatchewan Administration District and while there are no communities along its course, the towns of Big River and Spiritwood are in its watershed.
Christopher Lake is a recreational lake in the boreal forest ecozone in the Canadian province of Saskatchewan. It is located south-east of Emma Lake and Great Blue Heron Provincial Park in the central part of the province in the District of Lakeland No. 521. Access to Christopher Lake is from Highways 953 and 263 and it is about 42 km (26 mi) north of the city of Prince Albert.
Cypress Lake is an interbasin transfer reservoir in the Canadian province of Saskatchewan on the southern slopes of the Cypress Hills in the Rural Municipality of Reno No. 51. The reservoir was created by the damming of the east and west sides of a much smaller Cypress Lake in the late 1930s. There is a provincial recreation site on the southern shore and a wildlife refuge on Heglund Island in the lake. Access to the lake is from Township Road 60 off of Highway 21.
Bradwell Reservoir is a man-made reservoir in the Canadian province of Saskatchewan in the Rural Municipality of Blucher No. 343. The reservoir was built as part of the South Saskatchewan River Project. That project involved the damming of the South Saskatchewan River with the Gardiner and Qu'Appelle River Dams creating Lake Diefenbaker. From Lake Diefenbaker, a series of aqueducts were built allowing for irrigation and the creation of several reservoirs, including Bradwell Reservoir. The reservoir is owned and operated by the Saskatchewan Water Security Agency. Bradwell Reservoir supplies water to the Nutrien Allan Potash Mine near Allan.
Round Lake is a lake in the Canadian province of Saskatchewan within the Rural Municipality of Kelvington No. 366. The lake is at the western edge of the Porcupine Hills and Porcupine Provincial Forest in the Mid-Boreal Upland ecozone. It is 18 kilometres (11 mi) south of Greenwater Lake Provincial Park and 24 kilometres (15 mi) north-northeast of Kelvington. There are no communities along the lake's shore and access is from a gravel road off Highway 38.
