Nicoamen River

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The Nicoamen River is a tributary of the Thompson River in the southern Interior of British Columbia, Canada, located 15 kilometres (9 mi) upstream from its confluence with the Thompson at Lytton.

Thompson River river in British Columbia

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.

The British Columbia Interior, BC Interior or Interior of British Columbia, usually referred to only as the Interior, is one of the three main regions of the Canadian province of British Columbia, the other two being the Lower Mainland, which comprises the overlapping areas of Greater Vancouver and the Fraser Valley, and the Coast, which includes Vancouver Island and also including the Lower Mainland.

Canada Country in North America

Canada is a country in the northern part of North America. Its ten provinces and three territories extend from the Atlantic to the Pacific and northward into the Arctic Ocean, covering 9.98 million square kilometres, making it the world's second-largest country by total area. Canada's southern border with the United States, stretching some 8,891 kilometres (5,525 mi), is the world's longest bi-national land border. Its capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. As a whole, Canada is sparsely populated, the majority of its land area being dominated by forest and tundra. Consequently, its population is highly urbanized, with over 80 percent of its inhabitants concentrated in large and medium-sized cities, with 70% of citizens residing within 100 kilometres (62 mi) of the southern border. Canada's climate varies widely across its vast area, ranging from arctic weather in the north, to hot summers in the southern regions, with four distinct seasons.

The Nicoamen forms the extreme northeast boundary of the Cascade Mountains and part of the western boundary of the Thompson Plateau. Located nearby is the Nicoamen Plateau, a small subplateau of the Thompson Plateau.

Cascade Range mountain range in western North America

The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The latter term is also sometimes used by Washington residents to refer to the Washington section of the Cascades in addition to North Cascades, the more usual U.S. term, as in North Cascades National Park. The highest peak in the range is Mount Rainier in Washington at 14,411 feet (4,392 m).

Thompson Plateau

The Thompson Plateau, also known as the Okanagan-Thompson Plateau, forms the southern portion of the Interior Plateau of British Columbia, Canada, lying to the west of Okanagan Lake, south of the Thompson River and to the east of the Fraser River. At its most southern point the plateau is squeezed by the mountainous terrain of the Cascade Range abutting closer to the Okanagan Valley. Its southwestern edge abuts the Canadian Cascades portion of that extensive range, more or less following the line of the Similkameen River, its tributary the Tulameen River, and a series of passes from the area of Tulameen, British Columbia to the confluence of the Thompson River with the Nicoamen River, a few miles east of Lytton, British Columbia, which is in the Fraser Canyon. Its northeastern edge runs approximately from the city of Vernon, British Columbia through the valley of Monte Creek to the junction of the same name just east of the city of Kamloops. Northeast of that line is the Shuswap Highland.

The Nicoamen Plateau is a small sub-plateau of the Thompson Plateau in the southern Interior of British Columbia, Canada, located between the Nicoamen River (W) and the lower valley of the Nicola River (E).

History

The confluence of the Thompson and Nicoamen is the site of one of the incidents which led to the Fraser Canyon Gold Rush of 1858–60, as the location of a meet-up between the Nlaka'pamux people of the area and American miners.

Fraser Canyon Gold Rush

The Fraser Canyon Gold Rush, began in 1857 after gold was discovered on the Thompson River in British Columbia at its confluence with the Nicoamen River a few miles upstream from the Thompson's confluence with the Fraser River at present-day Lytton. The rush overtook the region around the discovery, and was centered on the Fraser Canyon from around Hope and Yale to Pavilion and Fountain, just north of Lillooet.

Nlakapamux ethnic group

The Nlaka'pamux or Nlakapamuk, also previously known as the Thompson, Thompson River Salish, Thompson Salish, Thompson River Indians or Thompson River people, and historically as the Klackarpun, Haukamaugh, Knife Indians and Couteau Indians, are an indigenous First Nations people of the Interior Salish language group in southern British Columbia. Their traditional territory includes parts of the North Cascades region of Washington.

Related Research Articles

The Kamloops Indian Band, also known as the Tk’emlups te Secwepemc, is one of the largest of the 17 groups into which the Secwepemc (Shuswap) nation was divided when the Colony of British Columbia established an Indian reserve system in the 1860s. The Kamloops Indian Band is a First Nations government within the Shuswap Nation Tribal Council, which represents ten of the seventeen Secwepemc band governments, all in the southern Central Interior region, spanning the Thompson and Shuswap districts.

Cariboo Plateau

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 Bonaparte Plateau, in British Columbia, Canada, is a subarea of the larger Cariboo Plateau which extends to the Quesnel River and lies between the Cariboo Mountains on the east and the Fraser River on the west. The Cariboo Plateau is a subarea of the Interior Plateau, aka the Fraser Plateau.

Camchin, also spelled Kumsheen, is an anglicization of the ancient name for the locality and aboriginal village once located on the site of today's Village of Lytton, British Columbia, Canada, whose name in the Nlaka'pamux language is ƛ'q'əmcín It also refers to the main Indian Reserve community of the Lytton First Nation adjacent to the Village of Lytton and is found in the form Kumsheen in local business and school names.

Coldwater River Provincial Park is a provincial park in British Columbia, Canada, located at the confluence of the Coldwater River with Cullet Creek, 50 km south of Merritt on BC Highway 5.

Silver Lake Provincial Park is a provincial park in British Columbia, Canada, located in the Skagit River Valley just south of Hope and comprising 77 ha.

Bonaparte Indian Band

The Bonaparte Indian Band a.k.a. Bonaparte First Nation, is a member band of the Shuswap Nation Tribal Council of the Secwepemc (Shuswap) people.

The Ashcroft First Nation is a First Nations government Thompson Canyon area of the Central Interior of the Canadian province of British Columbia. It's Indian Reserves are located near the town of Ashcroft, British Columbia, it is a member of the Nlaka'pamux Nation Tribal Council.

Quesnel Highland mountain in Canada

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.

The Lytton First Nation, a First Nations government, has its headquarters at Lytton in the Fraser Canyon region of the Canadian province of British Columbia. While it is the largest of all Nlaka'pamux bands, unlike all other governments of the Nlaka'pamux (Thompson) people, it is not a member of any of the three Nlaka'pamux tribal councils, which are the Nicola Tribal Association, the Fraser Canyon Indian Administration and the Nlaka'pamux Nation Tribal Council.

Hat Creek is a tributary of the Bonaparte River in British Columbia, Canada, joining that stream at Carquile, which is also known as Lower Hat Creek and is the site of the Hat Creek Ranch heritage museum and visitor centre. The Hat Creek basin includes a broad upper plateau area encircled by the gentle but high summits of the Clear Range and, to its east, the Cornwall Hills; this area is known as Upper Hat Creek. Adjacent to Upper Hat Creek is the gateway to Marble Canyon and a rancherie of the Pavilion First Nation, who are both a St'at'imc and Secwepemc people. During the Fraser Canyon and Cariboo Gold Rushes an important trail northwards from the lower Fraser Canyon led from Foster Bar on the Fraser via Laluwissen Creek into Upper Hat Creek, then via the creek to the Bonaparte River. The economy of the basin is ranching-based and includes some of the oldest ranches in the British Columbia Interior. On the northwest edge of the Upper Hat Creek basin there is a large lignite deposit and several exploratory pits, some dating back to the 19th century but some more recent, part of an intended, but now shelved Hat Creek coal-thermal proposal.

Cache Creek, originally Rivière de la Cache, is a tributary of the Bonaparte River in the Thompson Country of the Interior of British Columbia, Canada, joining that river at the town of Cache Creek, British Columbia, which is located at the junction of the Trans-Canada and Cariboo Highways.

Gitanyow

Gitanyow is an Indian reserve community of the Gitxsan people, located on the Kitwanga River 8 km south of Kitwancool Lake, at the confluence of Kitwancool Creek. The community is located on Gitanyow Indian Reserve No. 1.

The Inklin River is a river in northern British Columbia, Canada. It flows northwest into the head of the Taku River, which is formed by the convergence of the Inklin with the Nakina River, which flows southwest to meet it at the uninhabited locality of Inklin, which is located at the confluence.

The McGregor Plateau is a sub-plateau of the Fraser Plateau, the northernmost major subdivision of the Interior Plateau spanning the inland regions of the Pacific Northwest. Located in British Columbia, Canada, to the east of the city of Prince George, British Columbia, the McGregor Plateau lies between the main spine of the Northern Rocky Mountains on the east and the Fraser River on the west, beginning on its southeast at the confluence of the Torpy River with the Fraser and running northwest, parallel to the Fraser and the Rockies, to end in the area of the Arctic and Pacific Lakes to the north of the great bend in the Fraser River just upstream from and to the northeast of Prince George. The McGregor Plateau is very mountainous in character and includes several large rivers, the largest being the McGregor River and Herrick Creek. Included in the McGregor Plateau is the McGregor Range, which lies between the McGregor and Torpy Rivers.

The Deadwood River is a tributary of the Dease River in the far north of British Columbia, Canada. It forms the southeastern boundary of the Dease Plateau, which extends northward to the Yukon-British Columbia boundary and beyond.

Yale First Nation is a First Nations government located at Yale, British Columbia. Yale has 16 distinct reserves stretching from near Sawmill Creek to American Creek, with the most southern reserve situated at Ruby Creek in the District of Kent.

The Hackett River is a river in far northwestern British Columbia. It is a tributary of the Sheslay River, which is a feeder-stream of the Inklin River, the main southeast fork of the Taku. The locality of Sheslay is located at its confluence with the river of that name.

Atnarko is a locality on the Atnarko River, at the south end of Tweedsmuir Provincial Park in the Bella Coola Valley region of British Columbia, Canada. The original name of the post office located here was Anaham, a name associated with the Tsilhqot'in people of the neighbouring Chilcotin Country region. Opened under that name in 1907, it was changed to Atnarko in 1913, with the post office itself closing in 1932.

References

Coordinates: 50°16′00″N121°24′00″W / 50.26667°N 121.40000°W / 50.26667; -121.40000

Geographic coordinate system Coordinate system

A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.