Fir River | |
---|---|
Location | |
Country | Canada |
Province | Saskatchewan |
Rural municipality | RM of Hudson Bay No. 394 |
Physical characteristics | |
Source | Pasquia Hills |
• location | Wildcat Hill Provincial Park |
• coordinates | 53°13′47″N102°26′34″W / 53.229658°N 102.442852°W |
Mouth | Red Deer River |
• location | Hudson Bay Regional Park |
• coordinates | 52°49′07″N102°22′43″W / 52.818535°N 102.37850°W |
• elevation | 363 m (1,191 ft) |
Basin features | |
River system | Red Deer River drainage basin |
Tributaries | |
• right | Nonsuch Creek |
Fir River [1] is a river in the Canadian province of Saskatchewan. The river's source is in the east central part of the province in the heart of the Pasquia Hills, which is one of four landforms that make up the Manitoba Escarpment. It flows in a southward direction until it meets up with the Red Deer River south of the town of Hudson Bay in Hudson Bay Regional Park. The river is in the boreal forest. [2] Fir River is in the Nelson River drainage basin.
Fir River begins at a small lake in the south-east corner of Wildcat Hill Provincial Park in the Pasquia Hills. The lake is in a small valley just west of Bankside Lake, which flows into Man River. While Fir River heads south towards Red Deer River, Man River eventually makes its way northward and is in the Saskatchewan River watershed. Wildcat Hill ( 53°17′58″N102°29′01″W / 53.2995°N 102.4836°W ), while in the Man River watershed, is only about 6.5 kilometres (4.0 mi) north of Fir River's source. [3] The Pasquia River's source is just on the north-east side of Bankside Lake and it flows north-east and into the Saskatchewan River at The Pas, Manitoba. [4]
From Fir River's source, it flows southward towards Overflow Lake (the source of Overflowing River [5] ) where it turns north-west until it meets a valley. The river flows into the valley and heads south past several small lakes, including Bell, Chartier, Dagg, and Rat. As the river comes out of the hills, it passes through Fir River Road Recreation Site and Fir River Eco Reserve en route to Hudson Bay and the Red Deer River. As it approaches Hudson Bay, the land flattens out and it is met by Nonsuch Creek just north-west of town. At the mouth of the river, is Hudson Bay Regional Park, which features camping, golfing, [6] and picnicking. [7] The park is also the site of historical fur trading forts, most notably Fort Red Deer River. [8]
Fir River Road Recreation Site ( 53°04′56″N102°39′55″W / 53.0821°N 102.6653°W ) [9] is a provincial recreation park along Fir River and Fir River Road that is divided into two sections—one at mile marker 16 and the other at mile marker 21. Activities at the recreation site include picnicking, ATVing, fishing, and hunting. Brook trout can be found in the river. [10] In the winter, there are two warm-up shacks for snowmobilers that are maintained by the local snowmobile club. [11]
The recreation site also provides access to Fir River Ecological Reserve. [12]
Wollaston Lake is a lake in north-eastern Saskatchewan, Canada. It is 550 kilometres (340 mi) northeast of Prince Albert. With a surface area of 2,286 square kilometres (883 sq mi), it is the largest bifurcation lake in the world – that is, a lake that drains naturally in two directions.
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.
Little Bear Lake is a lake in the boreal forest ecozone in the Canadian province of Saskatchewan. The lake is in a hilly plateau called Cub Hills and the landforms, such as the lakes and streams, of the Cub Hills were formed over 10,000 years ago during the last ice age. Little Bear Lake is accessed from Hanson Lake Road, which runs along the eastern side of the lake, and by a small airport called Little Bear Lake Airport.
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.
Wildcat Hill Provincial Park is a wilderness park in north-eastern Saskatchewan approximately 40km from Hudson Bay. It is located amongst the Pasquia Hills, south of Highway 55, and west of Highway 9. The 21,752-hectare park was established as a protected area in 1971, and became a provincial park in 1992.
Mountain Cabin Recreation Site is a recreation site, and former settlement, near the north-eastern ridge of the Pasquia Hills in Canadian province of Saskatchewan.
Porcupine Hills Provincial Park is the newest provincial park in the Canadian Province of Saskatchewan. It was created in 2018 through the amalgamation of five pre-existing provincial recreation sites south-east of the town of Hudson Bay. The park is in the Porcupine Provincial Forest in the Porcupine Hills, which is a geographical feature in eastern Saskatchewan and western Manitoba. The hills are part of a range of hills called the Manitoba Escarpment.
Hudson Bay Regional Park is a regional park in the Canadian province of Saskatchewan. It is located on the south side of the town of Hudson Bay in the RM of Hudson Bay No. 394 along the shores of the Red Deer River. The park is the site of a North West Company fur trading fort called Fort Red Deer River that was built in 1790. About 14 kilometres (8.7 mi) downstream, near Erwood, was a Hudson's Bay Company trading post that was built in 1757.
Red Deer River is a river in the Canadian provinces of Saskatchewan and Manitoba. It has its source at Nut Lake in east central Saskatchewan and from there, it flows east towards Manitoba where it empties into Dawson Bay of Lake Winnipegosis. To the north of Red Deer's basin is the Saskatchewan River, to the south-west is the upper Assiniboine River, and to the south-east is Swan River.
Etomami River is a river in the Canadian province of Saskatchewan. The river originates in the Porcupine Hills and flows northward towards the town of Hudson Bay and into the Red Deer River. "Etomami" is a First Nations word that means "a place that three rivers join." It is in reference to the spot along the Red Deer River where the mouths of the Etomami and Fir Rivers meet the Red Deer River.
Pasquia Hills are hills in the Canadian province of Saskatchewan. They are located in the east central part of the province in the RM of Hudson Bay No. 394 near the Manitoba border. The hills are the northern most in a series of hills called the Manitoba Escarpment. The Manitoba Escarpment marks the western edge of the pre-historical glacial Lake Agassiz. The other four hills include Porcupine Hills, Duck Mountain, and Riding Mountain.
Hanson Lake is a lake in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. The lake is irregularly shaped with many bays, islands, and channels as it was formed by glaciers during the last ice age. It is fed by multiple rivers and creeks from surrounding hills, smaller lakes, and muskeg. Hanson Lake's outflow is through a short river at the eastern end of the lake as it flows into the Sturgeon-Weir River, a tributary of the Saskatchewan River.
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.
McBride Lake is a lake in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. It is a narrow lake that runs west to east along the course of the Pepaw River known for its fishing and recreational opportunities. It is situated in the Porcupine Hills and within Saskatchewan's Porcupine Provincial Forest. There is a provincial park and a small subdivision along the lake's shore and access is from Highway 983. Eldredge Lake is upstream from McBride Lake along the course of the Pepaw River and Pepaw Lake is downstream. Swallow lake is to the north and a short stream flows from Swallow Lake into the eastern end of McBride Lake.
Pepaw Lake, also spelt Peepaw and Pee Paw, is a lake in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. There is a provincial park on the eastern shore of the lake, and it is located at the junction of Highway 983 and Highway 982, which is also known as Little Swan Road. Access to the lake and the park is from Little Swan Road.
Saginas Lake, is a lake in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. It is located along the course of the Pepaw River and is situated in the Porcupine Hills. It is within Saskatchewan's Porcupine Provincial Forest and a portion of Porcupine Hills Provincial Park is on the eastern shore of the lake. Upstream along the Pepaw River is Pepaw and McBride Lakes—both of which lakes also have recreation sites that are part of Porcupine Hills Provincial Park. The lake and park are accessed from Highway 982, also known as Little Swan Road.
Parr Hill Lake, is a lake in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. It is part of the Swan River drainage basin and is situated in the Porcupine Hills and Saskatchewan's Porcupine Provincial Forest. A block of Porcupine Hills Provincial Park is on the north-eastern shore of the lake. The lake and park are accessed from Highway 982, which is also known as Little Swan Road.
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.
Piwei River is a river in the east-central part of the Canadian province of Saskatchewan in the boreal forest ecozone of Canada. It begins at the western end of the Porcupine Hills at Piwei Lakes and heads in an easterly direction through a glacier-formed valley and into the Etomami River, which is a tributary of the Red Deer River.
Woody River is a river in the Canadian provinces of Manitoba and Saskatchewan. The river's source is in the Porcupine Hills and Porcupine Provincial Forest of eastern Saskatchewan. From there it flows south through boreal forest and then east through Boreal Plains in the Parkland Region of Manitoba en route to Swan Lake. The river parallels the Swan River for much of its route as it travels through Swan River Valley between Duck Mountain and Porcupine Hills of the Manitoba Escarpment. Bowsman is the only notable community along the course of Woody River. Several highways cross it, including Saskatchewan's Highway 980, Manitoba's Roads 588, 587, 366, 268, and Manitoba's Highway 10.