Etomami Lake | |
---|---|
Location | RM of Preeceville No. 334 |
Coordinates | 52°15′20″N102°39′04″W / 52.2556°N 102.6512°W |
Type | Bifurcation lake |
Part of | Nelson River drainage basin |
River sources | Porcupine Hills |
Primary outflows | |
Basin countries | Canada |
Surface area | 19.3 ha (48 acres) |
Shore length1 | 4 km (2.5 mi) |
Surface elevation | 524 m (1,719 ft) |
Settlements | None |
1 Shore length is not a well-defined measure. |
Etomami Lake [1] [2] is a bifurcating lake in the east-central part of the Canadian province of Saskatchewan. The lake is in a glacier-carved valley in the Porcupine Hills within the Rural Municipality of Preeceville No. 334. It is the headwaters for both the Etomami and the Lilian Rivers. Henry Kelsey of the Hudson's Bay Company travelled past the lake in 1691 when he went from the Etomami River system to the Lilian.
Etomami is Cree for "where 3 rivers join" which is in reference to where the three rivers of Etomami, Red Deer, and Fir meet near the town of Hudson Bay. [3]
In 1691, Hudson's Bay Company fur trader and explorer Henry Kelsey traversed the natural portage between the Etomami and Lilian Rivers while in search of a route to the aspen parkland region. He had travelled south up the Etomami River from the Red Deer River to Etomami Lake where he crossed over to the Lilian River system. He was following a trail known to be used by the local Indigenous peoples. [4]
Etomami Lake is a small, narrow lake with an area of 48 hectares (120 acres) [5] and a shoreline of 4 kilometres (2.5 mi). [6] The lake sits in a glacial spillway in the Porcupine Hills of east-central Saskatchewan and has two outflows. The Etomami River [7] flows out of the north end of the lake where it meets the Red Deer River near the town of Hudson Bay. At the southern end of the lake is a swampy area that flows downstream into neighbouring Lilian Lake. [8] This is the source of the Lilian River [9] which, from there, heads in a southerly direction and meets the Assiniboine River at Sturgis. Both rivers are within the Nelson River watershed. The Canadian National Railway runs along the western shore of the lake through the valley while Highway 9 travels past the eastern shore above the valley.
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. 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 Assiniboine River is a 1,070-kilometre (660 mi) long river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle, Souris, and Whitesand Rivers.
Henry Kelsey was an English fur trader, explorer, and sailor who played an important role in establishing the Hudson's Bay Company in Canada.
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.
The Manitoba Escarpment, or the Western Manitoba Uplands, are a range of hills along the Saskatchewan–Manitoba border. The eastern slopes of the range are considered to be a scarp. They were created by glacial scouring and formed the western shore of prehistoric Lake Agassiz.
Touchwood Hills are a range of hills in the Canadian province of Saskatchewan. The hills are composed of the "Big" Touchwood Hills and the Little Touchwood Hills. Together they are referred to as the Touchwood Uplands. The hills are in the Prairie Pothole Region of North America, which extends throughout three Canadian provinces and five U.S. states, and within Palliser's Triangle and the Great Plains ecoregion of Canada.
Touchwood Hills Post Provincial Park is the location of a former Hudson's Bay Company (HBC) fur trading post that existed from 1879 to 1909 in the Touchwood Uplands of the Canadian province of Saskatchewan. In 1986, the site was designated a provincial park. It is located along Highway 15 in the RM of Kellross No. 247, about 10 kilometres (6.2 mi) west of Lestock and 16 kilometres (9.9 mi) east of Punnichy.
Red Deer Lake is a lake located in the west-central region of the Canadian province of Manitoba. The lake's primary inflow and outflow is the Red Deer River. It is situated approximately 8 kilometres (5.0 mi) north of Barrows and 16 kilometres (9.9 mi) west of Dawson Bay, which is part of the larger Lake Winnipegosis. The lake lies about 13 kilometres (8.1 mi) east of the Saskatchewan border.
Fur trading on the Assiniboine River and the general area west of Lake Winnipeg, in what is now Manitoba, Canada, began as early as 1731.
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.
Fir River 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. Fir River is in the Nelson River drainage basin.
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.
Armit River is a river in the Canadian provinces of Manitoba and Saskatchewan in the Nelson River drainage basin. The river begins in the Porcupine Hills of the Manitoba Escarpment at Armit Lake and flows in a northerly direction closely following the Manitoba / Saskatchewan border and into Red Deer Lake along the course of the Red Deer River.
Armit Lake is a lake in the Canadian provinces of Manitoba and Saskatchewan. The lake is about 50 kilometres (31 mi) north-northwest of Swan River, Manitoba, 62 kilometres (39 mi) east-southeast of Hudson Bay, Saskatchewan, and is situated in the Porcupine Hills of the Manitoba Escarpment. Most of the lake is in Manitoba with only the very western end across the border into Saskatchewan. With no public roads going to the lake, it is notoriously difficult to get to.
Lilian River is a river in the Canadian province of Saskatchewan. The river begins at Lilian Lake in the Porcupine Hills and flows south to join to the Assiniboine River at the town of Sturgis. Lilian Lake is connected to the bifurcating Etomami Lake via a natural swampy portage making Etomami Lake the headwaters for both the north flowing Etomami River and the south flowing Lilian River. For most of the river's length, it is followed by the Canadian National Railway (CNR) and Highway 9. Several small communities and parks are situated on or near the river's banks.