The Souris River or Mouse River is a river in central North America. Approximately 435 miles (700 km) in length, it drains about 23,600 square miles (61,100 km2) in Canada and the United States.
Emma Lake is a recreational lake in the Canadian province of Saskatchewan. It is located near the southern limit of the boreal forest, about 45 kilometres (28 mi) north of Prince Albert. The lake is within the District of Lakeland No. 521 and east of Prince Albert National Park. There are several small communities and recreational opportunities around Emma Lake and much of the northern half is within Great Blue Heron Provincial Park. Access to the lakes is from Highways 953, 952, and 263.
Alameda is a town in south-eastern Saskatchewan, Canada, approximately 50 km east of Estevan. A translation of Alameda from Spanish is "Poplar Grove" or "Tree Lined Avenue". One popular story is that the town was named for Alameda, California although there is no written documentation to support this. Alameda had a population of 369 in the Canada Census of 2016.
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. 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.
Highway 35 is a paved undivided provincial highway in the Canadian province of Saskatchewan.. It runs from the US Border near Port of Oungre to a dead end near the north shore of Tobin Lake. Saskatchewan Highway 35 (SK Hwy 35) is about 569 kilometres (354 mi) long. The CanAm Highway comprises Saskatchewan Highways 35, SK Hwy 39, SK Hwy 6, SK Hwy 3, SK Hwy 2 and U.S. Route 85. 74.6 kilometres (46.4 mi) of SK Hwy 35 contribute to the CanAm Highway between Port of Oungre on the Canada – United States border and Weyburn. Mudslides, and spring flooding were huge road building and maintenance problems around Nipawin as well as along the southern portion of the route named the Greater Yellow Grass Marsh. Over 20 early dams were built until the problem was addressed with the Rafferty-Alameda Project on the Souris River and the construction of the Qu'Appelle River Dam which have helped to eliminate washed out roads and flooded communities. The highway through the homesteading community followed the Dominion Land Survey on the square until reaching the Saskatchewan River at Nipawin. The completion of the combined railway and traffic bridge over the Saskatchewan River at Nipawin in the late 1920s retired the ferry and basket crossing for traffic north of Nipawin. The E.B. Campbell Dam built in 1963 northeast of Nipawin created Tobin Lake, and Codette Lake was formed with the construction of the Francois-Finlay Hydroelectric dam at Nipawin. The railway/traffic bridge that formed part of Highway 35 was the only crossing utilized at Nipawin until a new traffic bridge was constructed in 1974. The new bridge then became part of the combined Highway 35 and 55 until the highway parts just east of White Fox. Highway 35 then continued north along the west side of Tobin Lake. The railway/traffic bridge continues to be utilized for one lane vehicle traffic controlled by traffic lights, and continues as the "old highway 35" on the west side of the river until it joins with the current Highway 35/55.
Gleniffer Lake also known as Gleniffer Reservoir or originally Lake Gleniffer is an artificial lake in central Alberta, Canada created in 1983 by the construction of the Dickson Dam which impounded the Red Deer River, a major tributary of the South Saskatchewan River which flows into the Saskatchewan River Basin.
Boundary Dam Reservoir is a man-made lake in the south-east corner of the Canadian province of Saskatchewan. It is in census division 1, in the RM of Estevan. The closest city is Estevan, which is about 5.5 kilometres (3.4 mi) downstream. There are no towns or villages along the lake's shore but there are two subdivisions and a regional park. The subdivisions, which are in the RM of Estevan, are called Sunset Bay and Lakewood. The primary inflow and outflow for the reservoir is Long Creek. There is a 10-kilometre long diversion channel that goes to McDonald Lake that can take excess water in either direction.
Lake Darling Dam is an earthen embankment dam on the Souris River in the west north central United States, located twenty miles (30 km) northwest of Minot in Ward County, North Dakota. The dam began impounding water in April 1936 and was completed July of that year; it was created for the purposes of water storage and conservation.
The Whitesand River is a tributary of the Assiniboine River and finds its headwaters at Whitesand Lake near Invermay in east-central Saskatchewan. Its mouth can be found at its confluence with the Assiniboine River near Kamsack.
McDonald Lake, also known as Rafferty Reservoir, is a reservoir in south-east 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 km2 (5,000 sq mi). The upland rises about 200 m (660 ft) above the broad, flat prairie which is about 600 m (2,000 ft) above sea level. The highest peak is "Moose Mountain" at 830 m (2,720 ft) above sea level. The area 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."
Moosomin Lake, also known as Moosomin Reservoir, is a man-made lake in south-eastern part of the Canadian province of Saskatchewan. Created by the damming of Pipestone Creek in 1954, Moosomin Lake is located about 10 kilometres (6.2 mi) south of the town of Moosomin and is in the Souris River watershed. The reservoir's uses include irrigation, water supply, and recreation. Moosomin Lake Regional Park is on lake's western shore.
Long Creek is a river in central North America that begins in Saskatchewan, flows south-east into North Dakota, and then flows back north into Saskatchewan. It is a tributary of the Souris River. The Souris River drains into the Assiniboine River, which is part of the Red River drainage basin 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. In 1957, a dam was built on Long Creek near where it meets the Souris River to create Boundary Dam Reservoir.
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.
Moose Mountain Lake is a reservoir in the Canadian province of Saskatchewan. It is located in the RM of Golden West No. 95 in the Prairies Ecozone of Palliser's Triangle at the western edge of Moose Mountain Upland. Moose Mountain Creek is both the primary inflow and outflow of the lake; it enters at the north end and leaves at the dam in the south end. A secondary inflow that comes from Gooseberry Lake enters on the western side near the south end.
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.
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.
Crescent Creek is a river in the south-east region of the Canadian province of Saskatchewan. The river begins in the Beaver Hills and flows in an easterly direction into Crescent Lake. Crescent Creek is a tributary of Yorkton Creek, which flows north into the Whitesand River–a tributary of the Assiniboine River.
Anglin Lake is a reservoir in the boreal forest ecozone in the Canadian province of Saskatchewan. It is east of the Prince Albert National Park in the central part of the province in the District of Lakeland No. 521. Access to the lake is from Highway 953 and it is about 70 kilometres (43 mi) north of the city of Prince Albert. The only community on the lake is Anglin Lake.
Spruce River, also called Little Red River, is a river in the north-central region of the Canadian province of Saskatchewan. It begins in the Waskesiu Hills in Prince Albert National Park and flows generally in a southward direction through boreal forests, glacier carved hills and valleys, muskeg, and prairie en route to the North Saskatchewan River at the east end of the city of Prince Albert.
