Scum Lake (British Columbia)

Last updated
Scum Lake
Canada British Columbia relief location map.jpg
Red pog.svg
Scum Lake
Location of Scum Lake in British Columbia
Location Chilcotin District, British Columbia, Canada
Coordinates 51°47′09″N123°36′09″W / 51.78583°N 123.60250°W / 51.78583; -123.60250
Type Lake
Part of Pacific Ocean drainage basin
Primary outflows Haines Creek
Max. length2.2 km (1.4 mi)
Max. width0.6 km (0.37 mi)
Surface elevation1,189 m (3,901 ft)

Scum Lake is a lake in the Chilcotin region of the Interior of British Columbia, Canada. [1]

The major inflow, at the west, and outflow, at the northeast, is Haines Creek, which flows to the Chilcotin River near the settlement of Hanceville. The Chilcotin River flows via the Fraser River to the Pacific Ocean.

Scum Lake Airport is at the northeastern tip of the lake.

See also

Related Research Articles

<span class="mw-page-title-main">Chilcotin Group</span> Large area of basaltic lava in south-central British Columbia, Canada

The Chilcotin Group, also called the Chilcotin Plateau Basalts, is a large area of basaltic lava that forms a volcanic plateau running parallel with the Garibaldi Volcanic Belt in south-central British Columbia, Canada.

<span class="mw-page-title-main">Williams Lake, British Columbia</span> City in British Columbia, Canada

Williams Lake is a city in the Central Interior of British Columbia, in the central part of a region known as the Cariboo. Williams Lake is one of the largest cites, by population of metropolitan area, in the Cariboo after neighbouring Quesnel. The city is famous for the Williams Lake Stampede, which was once the second largest professional rodeo in Canada, after only the Calgary Stampede.

Chilcotin, meaning "people of the red ochre river" may refer to:

<span class="mw-page-title-main">Bridge River</span> River in British Columbia, Canada

The Bridge River is an approximately 120 kilometres (75 mi) long river in southern British Columbia. It flows south-east from the Coast Mountains. Until 1961, it was a major tributary of the Fraser River, entering that stream about six miles upstream from the town of Lillooet; its flow, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project, with the water now entering the Fraser just south of Lillooet as a result.

The Chilcotin region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River. Chilcotin is also the name of the river draining that region. In the language of the Tsilhqot'in people, their name and the name of the river means "those of the red ochre river". The proper name of the Chilcotin Country, or Tsilhqotʼin territory, in their language is Tŝilhqotʼin Nen.

<span class="mw-page-title-main">Chilcotin River</span> River in southern British Columbia, Canada

The Chilcotin River /tʃɪlˈkoʊtɪn/ located in Southern British Columbia, Canada is a 241 km (150 mi) long tributary of the Fraser River. The name Chilcotin comes from Tŝilhqot’in, meaning "ochre river people," where ochre refers to the mineral used by Tŝilhqot’in Nation and other Indigenous communities as a base for paint or dye. The Chilcotin River, Chilko River and Lake, and Taseko River and Lake make up the Chilcotin River watershed. This 19,200 km2 (7,400 sq mi) watershed drains the Chilcotin Plateau which reaches north to south from the Nechako Plateau to Bridge River county and east to west from Fraser River to the Coast Mountains. It is also one of twelve watersheds that make up the Fraser River Basin. Made up of seven major tributaries, Chilcotin River starts northeast of Itcha Mountain, flowing southeast until it joins the Fraser River south of Williams Lake, 22 km (14 mi) upstream from Gang Ranch.

<span class="mw-page-title-main">Tŝilhqox Biny</span> Lake in British Columbia, Canada

Tŝilhqox Biny, known as Chilko Lake, is a 180 km2 lake in west-central British Columbia, at the head of the Chilko River on the Chilcotin Plateau. The lake is about 65 km long, with a southwest arm 10 km long. It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation. It and Harrison Lake are the largest lakes in the southern Coast Mountains.

<span class="mw-page-title-main">Niut Range</span>

The Niut Range is 3600 km2 in area. It is a subrange of the Pacific Ranges of the Coast Mountains of British Columbia, although in some classifications it is considered part of the Chilcotin Ranges. The Niut is located in the angle of the Homathko River and its main west fork, Mosley Creek. It is isolated, island-like, by those rivers from its neighbour ranges, as both streams have their source on the Chilcotin Plateau in behind the range. Razorback Mountain is its highest peak.

<span class="mw-page-title-main">Homathko River</span> River in British Columbia, Canada

The Homathko River is one of the major rivers of the southern Coast Mountains of the Canadian province of British Columbia. It is one of the few rivers that penetrates the range from the interior Chilcotin Country to the coastal inlets of the Pacific Ocean. The Homathko River reaches the sea at the head of Bute Inlet, just west of the mouth of the Southgate River.

<span class="mw-page-title-main">Cariboo Plateau</span> Geographic feature in British Columbia, Canada

The Cariboo Plateau is a volcanic plateau in south-central British Columbia, Canada. It is part of the Fraser Plateau that itself is a northward extension of the North American Plateau. The southern limit of the plateau is the Bonaparte River although some definitions include the Bonaparte Plateau between that river and the Thompson, but it properly is a subdivision of the Thompson Plateau. The portion of the Fraser Plateau west of the Fraser River is properly known as the Chilcotin Plateau but is often mistakenly considered to be part of the Cariboo Plateau, which is east of the Fraser.

The Klinaklini River is one of the major rivers of the Pacific Ranges section of the Coast Mountains in the Canadian province of British Columbia. It originates in the Pantheon Range and empties into the head of Knight Inlet.

Scum Lake Airport, formerly TC LID: CAW3, was located adjacent to Scum Lake in Chilcotin District, British Columbia, Canada.

<span class="mw-page-title-main">Spruce Lake Protected Area</span> Protected natural area in British Columbia, Canada

The Spruce Lake Protected Area, formerly known variously as the Southern Chilcotin Mountains Provincial Park, Southern Chilcotins, and also as South Chilcotin Provincial Park, is a 71,347-hectare Protected Area in the British Columbia provincial parks system, approximately 200 km north of Vancouver. The area had been the subject of an ongoing preservationist controversy since the 1930s. In 2007, its status as a provincial park was downgraded to protected area.

The Taseko River or Dasiqox in the original Chilcotin, is a tributary of British Columbia's Chilko River, a tributary of the Chilcotin River which joins the Fraser near the city of Williams Lake.

<span class="mw-page-title-main">British Columbia Interior</span> Interior region of British Columbia, Canada

The British Columbia Interior, popularly referred to as the BC Interior or simply the Interior, is a geographic region of the Canadian province of British Columbia. While the exact boundaries are variously defined, the British Columbia Interior is generally defined to include the 14 regional districts that do not have coastline along the Pacific Ocean or Salish Sea, and are not part of the Lower Mainland. Other boundaries may exclude parts of or even entire regional districts, or expand the definition to include the regional districts of Fraser Valley, Squamish–Lillooet, and Kitimat–Stikine.

The Chilanko River is a river in the Chilcotin region of the Central Interior region of the Canadian province of British Columbia.

<span class="mw-page-title-main">Taseko Lakes</span> Group of lakes in British Columbia, Canada

The Taseko Lakes are a pair of lakes, Upper Taseko Lake and Lower Taseko Lake, which are expansions of the upper Taseko River in the southern Chilcotin District of the Central Interior of British Columbia, Canada. Their name is based on the original in the Chilcotin language, Dasiqox Biny, where "Desiqox" means "Mosquito River" and is cognate to the name of the river as in English; the Chilcotin name refers to both lakes as one lake, which was also originally the case with the English usage until official designation of the separate lakes in 1954. The lakes are separated by the short Taseko Narrows, the name of which in Chilcotin is nanats'akash, and is an important crossing place for deer. The Tchaikazan River flows the area between the upper & lower lake from the southwest, while the Taseko River feeds it from the southeast, while the equally large Lord River joins it from the south, at the head of the lake.

Scum Lake may refer to one of two lakes in Canada:

Itcha Lake is a lake in the Chilcotin District of the Central Interior of British Columbia, Canada. It is located northwest of Chilcotin Lake near the northeastern end of the Itcha Range in Itcha Ilgachuz Provincial Park.

References

  1. "Scum Lake". Geographical Names Data Base . Natural Resources Canada . Retrieved 2012-09-06.