The Saskatchewan River is a major river in Canada. It stretches about 550 kilometres (340 mi) from where it is formed by the joining together of the North Saskatchewan River and South Saskatchewan River just east of Prince Albert, Saskatchewan, to Lake Winnipeg. It flows roughly eastward across Saskatchewan and Manitoba to empty into Lake Winnipeg. Through its tributaries the North Saskatchewan and South Saskatchewan, its watershed encompasses much of the prairie regions of Canada, stretching westward to the Rocky Mountains in Alberta and north-western Montana in the United States.
The South Saskatchewan River is a major river in the Canadian provinces of Alberta and Saskatchewan. The river begins at the confluence of the Bow and Oldman Rivers in southern Alberta and ends at the Saskatchewan River Forks in central Saskatchewan. The Saskatchewan River Forks is the confluence of the South and North Saskatchewan Rivers and is the beginning of the Saskatchewan River.
Battle Creek is a river that begins in the south-eastern region of the Canadian province of Alberta, near the border with Saskatchewan, in the Cypress Hills Interprovincial Park. From Alberta, Battle Creek flows east and across the border into Saskatchewan. It flows south out of Saskatchewan across the Canada–United States border into Montana, where it joins the Milk River in Blaine County, Montana.
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.
Lake Diefenbaker is a reservoir and bifurcation lake in southern part of the Canadian province of Saskatchewan. It was formed by the construction of Gardiner Dam and the Qu'Appelle River Dam across the South Saskatchewan and Qu'Appelle Rivers respectively. Construction began in 1959 and the lake was filled in 1967. The lake is 225 kilometres (140 mi) long with approximately 800 kilometres (500 mi) of shoreline. It has a maximum depth of 66 metres (217 ft), while the water levels regularly fluctuate 3–9 metres (9–27 feet) each year. Lake Diefenbaker provides water for domestic irrigation and town water supplies. The flow of the two rivers is now regulated with a considerable portion of the South Saskatchewan diverted into the Qu'Appelle. Prior to the dams' construction, high water levels in the South Saskatchewan would frequently cause dangerous ice conditions downstream in Saskatoon while the Qu'Appelle would frequently dry up in the summer months.
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) 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.
The Quill Lakes is a wetland complex in Saskatchewan, Canada that encompasses the endorheic basin of three distinct lake wetlands: Big Quill Lake, Middle Quill Lake, and Little Quill Lake. On May 27, 1987, it was designated a wetland of international importance via the Ramsar Convention. It was the first Canadian site in the North American Waterfowl Management Plan, is a site in the International Biological Programme and Saskatchewan Heritage Marsh Program, and was designated a Western Hemisphere Shorebird Reserve Network site of International significance in May, 1994. The site is an important staging and breeding area for spring and fall migration of shorebirds. The site qualifies as an Important Bird Area (IBA) of Canada for its globally and nationally significant migratory and breeding populations of more than a dozen species of birds. The IBA is designated as Quill Lakes .
Lenore Lake is a partly saline lake in the Canadian province of Saskatchewan. It is part of the Lenore Lake Basin, which includes several saline lakes as well as the freshwater St. Brieux and Burton Lakes. The basin has no natural outlet. The lake is within the aspen parkland ecozone of Saskatchewan. Lenore Lake was designated a migratory bird sanctuary in 1925. Raven Island, located at the southern end of Lenore Lake, is a National Wildlife Area of Canada.
The Rural Municipality of Milden No. 286 is a rural municipality (RM) in the Canadian province of Saskatchewan within Census Division No. 12 and SARM Division No. 5.
Blackstrap Lake is a man-made reservoir in central Saskatchewan, Canada, south of Saskatoon in the Rural Municipality of Dundurn No. 314. The lake was created as a reservoir in 1967, as part of the Saskatoon South East Water Supply System. Blackstrap Lake has an area of 1,200 ha and is generally used to support irrigation, and the industrial and municipal water supply.
Indi Lake is a man-made lake in central Saskatchewan, Canada, south of Saskatoon in the Rural Municipality of Dundurn No. 314. The lake was created for irrigation and recreation in 1967 by a dam located at its south end. The lake is part of a greater irrigation and aqueduct system built in the 1960s in Saskatchewan and was named after Indi, an unincorporated railway point nearby on the Canadian National Railway (CNR).
Whitewater Lake is a lake in the Canadian province of Manitoba located between Boissevain and Deloraine. It is an endorheic basin and more marsh than lake. Whitewater Lake was previously called White Lake due to the color of the salt flats exposed during dry periods. Whitewater Lake covers approximately 22,000 acres on average and only reaches depths of about 2 metres (6.6 ft). The lake is fed by several small streams which flow into it from the Turtle Mountains but has no natural outflow.
Last Mountain Lake National Wildlife Area is a National Wildlife Area (NWA) in the Canadian province of Saskatchewan. The protected area is in 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 site is an Important Bird Area (IBA) of Canada, designated as Last Mountain Lake NWA .
Brightwater Creek is a river in south central part of the Canadian province of Saskatchewan. It is a tributary of the South Saskatchewan 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. Along the river's course there is a dam and reservoir and a regional park. There are no communities along its course.
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.
Oak Lake is a lake in the south-western part of the Canadian province of Manitoba in a region called Westman. Oak Lake is a kettle lake and is an aquifer supplier for numerous nearby residential areas and farms. The lake is in the RM of Sifton and sits at an elevation of 426 metres above sea level. Provincial Road 254 provides access to the lake.
Eyebrow Lake is a man-made marshy lake that parallels the Qu'Appelle River in the southern region of the Canadian province of Saskatchewan. Located in the RM of Huron No. 223, it is the first lake in a series of lakes along the Qu'Appelle River after Qu'Appelle River Dam and Lake Diefenbaker. The next lake downstream is Buffalo Pound Lake. The closest community is the village of Tugaske and while there are no public recreation sites at the lake, it can be accessed by Highway 627. The lake gets its name from the nearby Eyebrow Hills, which are shaped like an eyebrow. The nearby town of Eyebrow and RM of Eyebrow No. 193 are also named after these hills.
Maple Creek is a river in the south-west region of the Canadian province of Saskatchewan. The river is in the semi-arid region known as Palliser's Triangle. It begins in the Cypress Hills and flows generally in a northward direction and empties into the endorheic Bigstick Lake. The town of Maple Creek is the only notable community along the course of the river. Due to the generally dry and drought-prone conditions of the area, reservoirs were built along the river's course and in its watershed to ensure a stable water supply for irrigation. Two Important Bird Areas (IBA) of Canada cover much of the lower watershed of the river.
Reid Lake, also known as Duncairn Reservoir, is a man-made reservoir in the Canadian Province of Saskatchewan. Reid Lake was formed with the construction of the Duncairn Dam in a glacial meltwater channel along the course of Swift Current Creek in 1942. The reservoir was originally built to supply water for the city of Swift Current, for irrigation projects, and to regulate Swift Current Creek levels downstream. The entire lake is part of the Duncairn Reservoir Migratory Bird Sanctuary.
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