Williams Lake (British Columbia)

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Williams Lake
Canada British Columbia relief location map.jpg
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Williams Lake
Location British Columbia
Coordinates 52°07′01″N122°04′19″W / 52.11694°N 122.07194°W / 52.11694; -122.07194
Primary inflows San Jose River
Primary outflows Williams Lake River
Catchment area 2,240 km2 (860 sq mi)
Basin  countriesCanada
Max. length7.2 km (4.5 mi)
Max. width1.3 km (0.81 mi)
Surface area7.2 km2 (2.8 sq mi)
Average depth12.2 m (40 ft)
Max. depth24.1 m (79 ft)
Water volume0.088 km3 (71,000 acre⋅ft)
Residence time ca. 1.9 years
Surface elevation565 m (1,854 ft)
Settlements Williams Lake

Williams Lake is a lake in the city of the same name in the Cariboo region of the Central Interior of British Columbia, Canada. Williams Lake Indian Reserve No. 1, a.k.a. "Sugarcane Reserve" is located around the east end of the lake. British Columbia provincial highway 97, the Cariboo Highway, runs along the lake's northern side.

Contents

It is fed by the northwest-flowing San Jose River and drained to the Fraser River via the Williams Lake River. [1]

Climate and Hydrography

Williams Lake has relatively lower water temperatures, because of its lower elevation compared to other lakes on the Cariboo Plateau.

See also

Related Research Articles

Highway 97 is a major highway in the Canadian province of British Columbia. It is the longest continuously numbered route in the province, running 2,081 km (1,293 mi) and is the only route that runs the entire north–south length of British Columbia, connecting the Canada–United States border near Osoyoos in the south to the British Columbia–Yukon boundary in the north at Watson Lake, Yukon.

<span class="mw-page-title-main">British Columbia Highway 20</span> Highway in British Columbia

Highway 20, also known as the Chilcotin Highway, and officially dubbed the Alexander MacKenzie Highway, is one of the two main east–west routes in the Central Interior of British Columbia (the other being Highway 16. The Chilcotin Highway runs 457 km from Williams Lake westward through the Chilcotin region to North Bentinck Arm, an inlet from the Pacific Ocean where the town of Bella Coola is located. As of 2019, all but 42 km has been paved, mostly for expediting the removal of timber from the region, which, like most of British Columbia, is afflicted with pine beetle infestations. Logging traffic and ranch-related traffic on the route can be expected.

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

The Thompson River is the largest tributary of the Fraser River, flowing through the south-central portion of British Columbia, Canada. The Thompson River has two main branches, the South Thompson River and the North Thompson River. The river is home to several varieties of Pacific salmon and trout. The area's geological history was heavily influenced by glaciation, and the several large glacial lakes have filled the river valley over the last 12,000 years. Archaeological evidence shows human habitation in the watershed dating back at least 8,300 years. The Thompson was named by Fraser River explorer, Simon Fraser, in honour of his friend, Columbia Basin explorer David Thompson. Recreational use of the river includes whitewater rafting and angling.

<span class="mw-page-title-main">Index of British Columbia–related articles</span>

The following is an alphabetical list of articles related to the Canadian province of British Columbia.

<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.

<span class="mw-page-title-main">Cariboo Road</span> Historical route in British Columbia, Canada

The Cariboo Road was a project initiated in 1860 by the Governor of the Colony of British Columbia, James Douglas. It was built in response to the Cariboo Gold Rush to facilitate settlement of the area by miners. It involved a feat of engineering stretching from Fort Yale to Barkerville, B.C. through extremely hazardous canyon territory in the Interior of British Columbia.

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

The Fraser Canyon is a major landform of the Fraser River where it descends rapidly through narrow rock gorges in the Coast Mountains en route from the Interior Plateau of British Columbia to the Fraser Valley. Colloquially, the term "Fraser Canyon" is often used to include the Thompson Canyon from Lytton to Ashcroft, since they form the same highway route which most people are familiar with, although it is actually reckoned to begin above Williams Lake at Soda Creek Canyon near the town of the same name.

<span class="mw-page-title-main">Bowron Lake Provincial Park</span> Wilderness park in British Columbia, Canada

Bowron Lake Provincial Park is a wilderness provincial park located in east-central British Columbia, Canada, near the border with Alberta. It is 117 km (73 mi) east of the city of Quesnel. Other nearby towns include Wells and the historic destination of Barkerville. Once a popular hunting and fishing destination, today the park is protected and known for its abundant wildlife, rugged glaciated mountains, and freshwater lakes.

Williams Lake Indian Reserve, also called the Williams Lake First Nation or the Williams Lake Band Reservation and commonly referred to locally as the Sugarcane Reserve, aka Sugarcane or The Cane or SCB, is an Indian reserve in British Columbia, Canada, located at the east end of Williams Lake and 12 km east of the city of the same name, on the right bank of the San Jose River. and is home to the Williams Lake Indian Band. The band is part of the Northern Shuswap Tribal Council, also known as the Cariboo Tribal Council, which is one of two tribal councils of the Secwepemc peoples.

<span class="mw-page-title-main">Port Douglas, British Columbia</span> Place in British Columbia, Canada

Port Douglas, sometimes referred to simply as Douglas, is a remote community in British Columbia, Canada at east of the mouth of the Lillooet River, and at the head of Harrison Lake, which is the head of river navigation from the Strait of Georgia. Port Douglas was the second major settlement of any size on the British Columbia mainland during the Fraser Canyon Gold Rush. It came into being in 1858 when Governor Douglas ordered that it be laid out.

Cariboo was one of the twelve original electoral districts created when British Columbia became a Canadian province in 1871. Roughly corresponding to the old colonial electoral administrative district of the same name, it was a three-member riding until the 1894 election, when it was reduced through reapportionment and became a two-member riding until the 1916 election, after which it has been a single-member riding. It produced many notable Members of the Legislative Assembly (MLAs), including George Anthony Boomer Walkem, third and fifth holder of the office of Premier of British Columbia and who was one of the first representatives elected from the riding; John Robson, ninth Premier of British Columbia; and Robert Bonner, a powerful minister in the W.A.C. Bennett cabinet, and later CEO of MacMillan Bloedel and BC Hydro.

Alexander Vaughan Fraser was a Canadian politician. Fraser began his career as a businessman in the central British Columbia town of Quesnel, located in the Cariboo region. During World War II, he enlisted and served in the Royal Canadian Army Service Corps in British Columbia and Ontario from 1942 until his discharge in March 1946.

<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 Williams Lake First Nation is a First Nations government of the Secwepemc (Shuswap) Nation, located in the Cariboo region of the Central Interior region of the Canadian province of British Columbia, at the city of Williams Lake. It was created when the government of the then-Colony of British Columbia established an Indian reserve system in the 1860s. It is a member government of the Northern Shuswap Tribal Council. Its main Indian Reserve is Williams Lake Indian Reserve No. 1, a.k.a. "Sugarcane" or "The Cane" or "SCB".

<span class="mw-page-title-main">Quesnel Highland</span>

The Quesnel Highland is a geographic area in the Central Interior of the Canadian province of British Columbia. As defined by BC government geographer in Landforms of British Columbia, an account and analysis of British Columbia geography that is often cited as authoritative, the Highland is a complex of upland hill and plateau areas forming and defined as being the buffer between the Cariboo Plateau and the Cariboo Mountains, as a sort of highland foothills along the eastern edge of the Interior Plateau running southeast from a certain point southeast of the city of Prince George to the Mahood Lake area at the southeast corner of the Cariboo. Beyond Mahood Lake lies another separately classified area dubbed by Holland the Shuswap Highland which spans similar terrain across the North Thompson and Shuswap Lake-Adams River drainage basins, forming a similar upland-area buffer between the Thompson Plateau and the Monashee Mountains. A third area, the Okanagan Highland, extends from the southern end of the Shuswap Highland in the area of Vernon and Enderby in the northern Okanagan region into Washington State, and also abuts the Monashee Mountains.

<span class="mw-page-title-main">Shuswap Highland</span>

The Shuswap Highland is a plateau-like hilly area of 14,511 km2 (5,603 sq mi) in British Columbia, Canada. It spans the upland area between the Bonaparte and Thompson Plateaus from the area of Mahood Lake, at the southeast corner of the Cariboo Plateau, southeast towards the lower Shuswap River east of Vernon in the Okanagan.

The Ministry of Transportation and Infrastructure is the British Columbia government ministry responsible for transport infrastructure and law in the Canadian province of British Columbia. It is currently led by Rob Fleming.

<span class="mw-page-title-main">Fountain, British Columbia</span>

Fountain is an unincorporated rural area and Indian reserve community in the Fraser Canyon region of British Columbia, Canada, located at the ten-mile (16 km) mark from the town of Lillooet on BC Highway 99, which in that area is also on the route of the Old Cariboo Road and is located at the junction of that route with the old gold rush-era trail via Fountain Valley and the Fountain Lakes.

Pemberton Pass, 505 m (1,657 ft), also formerly known as Mosquito Pass, is the lowest point on the divide between the Lillooet and Fraser River drainages, located at Birken, British Columbia, Canada, in the principal valley connecting and between Pemberton and Lillooet. The pass is a steep-sided but flat-bottomed valley adjacent to Mount Birkenhead and forming a divide between Poole Creek, a tributary of the Birkenhead River, which joins the Lillooet at Lillooet Lake, and the Gates River which flows northeast from Gates Lake, at the summit of the pass, which flows to the Fraser via Anderson and Seton Lakes and the Seton River.

The Tanzilla River is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada.

References