Moose Mountain Creek | |
---|---|
Location | |
Countries | Canada |
Province | Saskatchewan |
Communities | |
Physical characteristics | |
Source | Chapleau Lakes, near Montmartre |
• location | Saskatchewan |
• elevation | 668 m (2,192 ft) |
Mouth | Souris River |
• location | South-west of Oxbow, Saskatchewan |
• coordinates | 49°12′55″N102°11′47″W / 49.21537°N 102.19634°W |
• elevation | 512 m (1,680 ft) |
Discharge | |
• location | Souris River, west of Oxbow |
Basin features | |
River system | Red River drainage basin |
Tributaries | |
• left | Wolf Creek, Crooked Creek, Swift Creek |
• right | Morrison Creek, Cowper Creek, Shepherd Creek |
[1] [2] |
Moose Mountain Creek is a river [3] 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. [4]
The entirety of Moose Mountain Creek is in Census Division No. 1. The river passes through two Indian reserves, Ocean Man and Pheasant Rump, and eight rural municipalities: Montmartre, Chester, Golden West, Tecumseh, Brock, Moose Mountain, Moose Creek, and Enniskillen. [5] While there are no communities along the banks of the river, there are four within two kilometres of its banks: Montmartre, Kisbey, Alameda, and Oxbow. The original location of Carlyle, NW 26-07-03 W2, was located near confluence of Moose Mountain, Swift, and Morrison Creeks.
Moose Mountain Creek flows generally in a south-easterly direction, starting north-west of Moose Mountain Upland and ending up at the Souris River near Oxbow. The western and southern regions of Moose Mountain fall within the river's watershed, which is part of the Upper Souris watershed. The northern most point of Moose Mountain Creek's watershed is near McLean, which is only 41 kilometres (25 mi) away from Saskatchewan's capital, Regina. [6] [7]
There are two major dams along the river. The first one is Moose Mountain Dam and the second is Grant Devine Dam, both of which created large reservoirs along the course. Both reservoirs have parks; Lost Horse Hills is on Moose Mountain Lake and Moose Creek Regional Park [8] is on Grant Devine Reservoir.
The Chapleau Lakes [9] are a chain of two lakes that run diagonally in a valley north to east. The northern most of the two lakes is the source of Moose Mountain Creek. From the outflow of that lake near Highway 48 and Highway 606, the river travels in a south-easterly direction until passes through the Saint Clair National Wildlife Area and Highway 711. From there, it empties into Moose Mountain Lake, which is a man-made reservoir. [10] Moose Mountain Dam, which was built in 1937, is at the south-east corner of the lake, near Lost Horse Hill. From there, the river continues to flow south-east through Ocean Man Indian Reserve then Pheasant Rump Indian Reserve until it crosses Highway 13 about half-way between Forget and Kisbey, where it takes a more easterly route. It's around this area, west, south, and east of Kisbey, that the river's course flattens out creating a broad floodplain. Dykes and culverts were built south of Kisbey to protect the village and control the river's flow. South of Forget, there were also culverts and other flood control measures built to control surface water before it reaches the river. From south of Kisbey, the river roughly parallels Highway 13 towards Arcola where it leaves the floodplain and flows into a valley, the Moose Mountain Creek Spillway. It continues east until it crosses Highway 9, at which point it takes a more southerly route and flows into a Grant Devine Reservoir. In 1994, the Alameda Dam was built along Moose Mountain Creek's course, near the point where it meets the Souris River, creating a large reservoir called Alameda Reservoir. In 2017, the name of the reservoir and dam were changed to Grant Devine Dam and Grant Devine Reservoir, in honour of the premier of Saskatchewan who was responsible for its construction, Grant Devine. Moose Mountain Creek is the primary inflow and outflow of the reservoir and meets the Souris River [11] about three miles south of the dam in the Souris River Valley, near the town of Oxbow.
Moose Mountain Creek Spillway is a valley that was formed during the last ice age as the path taken by melting glacial waters between two glacial lobes, the Weyburn Lobe and the Moose Mountain Lobe, en route to the Souris Spillway. On the southern side of Moose Mountain Upland, in the interlobate area, a short lived glacial lake named Lake Arcola formed along the current path of Moose Mountain Creek. Glacial moraines can be found throughout the area. [12]
Saint Clair National Wildlife Area ( 49°58′01″N103°06′34″W / 49.9669°N 103.1094°W ) is one of 27 Prairie National Wildlife Areas in Saskatchewan. [20] The park is at the northern end of Moose Mountain Lake, on the north side of Highway 711, about three miles west of the Highway 47 and 711 intersection. Moose Mountain Creek cuts through the park from the north-east to the south-west corner at which point it goes under Highway 711 and into the lake. It is about one square mile in size and sits in the valley at the confluence of Moose Mountain and an unnamed creek that comes in from the west. [21]
The Gardiner Dam on the South Saskatchewan River in Saskatchewan is the third largest embankment dam in Canada and one of the largest embankment dams in the world. Construction on Gardiner Dam and the smaller Qu'Appelle River Dam was started in 1959 and completed in 1967, creating Lake Diefenbaker upstream and diverting a considerable portion of the South Saskatchewan's flow into the Qu'Appelle River. The dam rises 64 metres (209 feet) in height, is almost 5 km (3.1 mi) long and has a width of 1.5 km (0.93 mi) at its base with a volume of 65,000,000 cubic meters. The dam is owned and operated by the Saskatchewan Water Security Agency.
The Antler River is located in the Prairie Pothole Region of North America's Great Plains in south-eastern Saskatchewan and south-western Manitoba in Canada in an area known as Palliser's Triangle. Its source is in Saskatchewan's Moose Mountain Upland and it is a major tributary of the Souris River. As a result, its flood levels are monitored by the United States Geological Survey.
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.
Wascana Creek is a river in the Canadian province of Saskatchewan. It is a tributary of the Qu'Appelle River.
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).
Waterhen River is an east-flowing river in the north-west area of the Canadian province of Saskatchewan in the drainage basin of the Beaver River. It is north of and parallel to the east-flowing part of the Beaver River and joins the north-flowing part of that river. Most of the river and its drainage basin is at the southern edge of the boreal forest belt. While the river's source is Lac des Îles, its drainage basin reaches north into the Mostoos Hills and west well into the neighbouring province of Alberta.
Nanaimo River is a river on Vancouver Island, British Columbia, Canada, located near the city of Nanaimo on the island's east coast. Its headwaters are in the Vancouver Island Ranges of central Vancouver Island and its mouth, the Nanaimo River estuary, is at the south end of Nanaimo Harbour in the Strait of Georgia. The estuary is part of the Pacific Estuary Conservation Program.
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.
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.
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.
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.
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.
Oak Lake is a lake in the southwestern region of the Canadian province of Manitoba.
Plum Creek is the primary outflow for the Plum Lakes and travels in an easterly direction for about 28 kilometres until it meets up with the Souris River, which is part of the Hudson Bay drainage basin, at the community of Souris in the Canadian province of Manitoba. Plum Lakes and the beginning of Plum Creek are in the Rural Municipality of Sifton and the mouth is in the Municipality of Souris – Glenwood.
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.
First Mustus Lake is a lake in Meadow Lake Provincial Park in the Canadian Province of Saskatchewan in the boreal forest ecozone of Canada. The lake is the first of four lakes in a row named Mustus in the Rusty Creek watershed. The other lakes are Second, Third, and Fourth Mustus. Rusty Creek and the lakes are part of the Waterhen River drainage basin. The Waterhen River is a tributary of the Beaver River, which flows north into Lac Île-à-la-Crosse and the Churchill River, a major tributary in the Hudson Bay drainage basin. Highway 224 provides access to both First and Second Mustus Lakes.
White Bear (Carlyle) Lake is a closed-basin lake in the Moose Mountain Upland. It is the largest lake on the plateau, slightly larger than its neighbour, Kenosee Lake. White Bear (Carlyle) Lake is within the White Bear 70 Indian reserve and Carlyle Lake Resort is along the southern shore. The lake and its amenities are accessed from Highway 9.
The Cub Hills are a hilly plateau located south-east of the geographical centre of the Canadian province of Saskatchewan. The hills are in the boreal forest ecozone of Canada and the landforms of the hills were shaped more than 10,000 years ago during last ice age. Throughout the Cub Hills, there are dozens of lakes and rivers and several parks. The Cubs Hills are 150 km (93 mi) north-east of Prince Albert and are in the Northern Saskatchewan Administration District and Census Division #18. Several highways criss-cross the plateau to provide access to the various parks and other amenities.
Pepaw River, also spelt Peepaw, is a river in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. It begins in the Porcupine Hills and flows northward and meets up with the Etomami River south of the town of Hudson Bay. Much of the river is within Saskatchewan's Porcupine Provincial Forest and as such has various recreational opportunities along its course.