The Saskatchewan River is a major river in Canada. It stretches about 550 kilometres (340 mi) from where it is formed by the joining 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 Mackenzie River is a river in the Canadian boreal forest. It forms, along with the Slave, Peace, and Finlay, the longest river system in Canada, and includes the second largest drainage basin of any North American river after the Mississippi.
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.
Lake Athabasca is in the north-west corner of Saskatchewan and the north-east corner of Alberta between 58° and 60° N in Canada. The lake is 26% in Alberta and 74% in Saskatchewan.
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.
Pipestone Creek is a waterway that runs through central Alberta, Canada. For example, over 100 acres (0.40 km2) of Pipestone Creek parkland is situated in Millet, Alberta, with a combination of meadows and urban forest.
The Sturgeon River is a 260-kilometre-long (160 mi) river in central Alberta. It is a major tributary of the North Saskatchewan River. The river crosses Sturgeon County, which was named for this river. For much of its length, the Sturgeon is the northwestern-most major river in the Hudson Bay drainage basin, as the river runs close to and parallel to the Arctic Divide.
The North Saskatchewan River is a glacier-fed river that flows from the Canadian Rockies continental divide east to central Saskatchewan, where it joins with the South Saskatchewan River to make up the Saskatchewan River. Its water flows eventually into the Hudson Bay.
The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into the Hudson Bay and adjoining waters. Spanning an area of about 3,861,400 square kilometres (1,490,900 sq mi) and with a mean discharge of about 30,900 m3/s (1,090,000 cu ft/s), the basin is almost entirely within Canada. It encompasses parts of the Canadian Prairies, Central Canada, and Northern Canada. A small area of the basin is in the northern part of the Midwestern United States.
Beaver River is a large river in east-central Alberta and central Saskatchewan, Canada. It flows east through Alberta and Saskatchewan and then turns sharply north to flow into Lac Île-à-la-Crosse on the Churchill River which flows into Hudson Bay.
Pigeon Lake is a lake in central Alberta, Canada that straddles the boundary between Leduc County and the County of Wetaskiwin No. 10. It is located close to Edmonton, Leduc and Wetaskiwin. Communities located along the lakeshore include Pigeon Lake Indian Reserve 138A, ten summer villages, and four unincorporated communities.
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.
Manitou Lake is a salt lake located mostly in the RM of Manitou Lake No. 422 in the Canadian province of Saskatchewan, about 10 kilometres (6.2 mi) east of the provincial border with Alberta. The eastern shore of the lake is in the RM of Hillsdale No. 440. Manitou Lake is located 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. Manitou Lake is part of an Important Bird Area (IBA) of Canada that covers 699.66 km2 (270.14 sq mi) of land and serval neighbouring lakes.
Coal Lake is a long, sinuous lake located approximately 60 km (37 mi) southeast of the city of Edmonton, just northeast of the city of Wetaskiwin. The lake is in one of the glacial meltwater channels formed when the 4,000 km2 (1,500 sq mi) of Lake Edmonton, which existed for roughly 100 years at the end of the last ice age, breached its ice dam and drained within a few weeks. The entire meltwater channel starts east of Nisku, wandering southeast through minor depressions and the chain of Saunders Lake, Ord Lake, three small unnamed lakes, Coal Lake and Driedmeat Lake.
Driedmeat Lake is a long ribbon lake in Alberta; part of the Battle River system. Its northern end is located approximately 10 km (6.2 mi) south of the city of Camrose. The city draws its water supply from the lake. It was originally created by a glacial meltwater channel, which carved the surrounding valley. In the valley and around it, Saskatoon berries, an ingredient of pemmican, grow and are endemic in the area.
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.
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.
Eyehill Creek is a river in the Canadian provinces of Alberta and Saskatchewan. The river begins at Sounding Lake in Alberta and flows east and north into Manitou Lake in Saskatchewan. Eyehill Creek is the primary inflow for Manitou Lake, which has no outflow. The Manitou Lake watershed is a large endorheic basin between the Battle River watershed to the north and the South Saskatchewan River watershed to the south.
