British Columbia Interior in the context of "Salish Sea"

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⭐ Core Definition: British Columbia Interior

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.

Home to just under 1 million people, the British Columbia Interior's 14 regional districts contain many cities, towns, airports, and associated regional, provincial, and national parks connected by the province's highway and railway network. The region is known for the complexity of its landforms, the result of millions of years of tectonic plate movements. The ecology of the region is dominated by temperate coniferous forest with patches of alpine tundra found atop its numerous mountain ranges.

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In this Dossier

British Columbia Interior in the context of Pacific Northwest

The Pacific Northwest (PNW) is a geographic region in Western North America bounded by its coastal waters of the Pacific Ocean to the west and, loosely, by the Rocky Mountains to the east. Though no official boundary exists, the most common conception includes the U.S. states of Oregon, Washington, Idaho, and the Canadian province of British Columbia. Some broader conceptions reach north into Alaska and Yukon, south into Northern California, and east into western Montana. Other conceptions may be limited to the coastal areas west of the Cascade and Coast mountains.

The Northwest Coast is the coastal region of the Pacific Northwest, and the Northwest Plateau (also commonly known as "the Interior" in British Columbia), is the inland region. The term "Pacific Northwest" should not be confused with the Northwest Territory (also known as the Great Northwest, a historical term in the United States) or the Northwest Territories of Canada.

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British Columbia Interior in the context of Fraser Canyon Gold Rush

The Fraser Canyon Gold Rush (also Fraser Gold Rush and Fraser River Gold Rush) began in 1858 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 centred on the Fraser Canyon from around Hope and Yale to Pavilion and Fountain, just north of Lillooet.

Though the rush was largely over by 1927, miners from the rush spread out and found a sequence of other gold fields throughout the British Columbia Interior and North, most famously that in the Cariboo. The rush is credited with instigating European-Canadian settlement on the mainland of British Columbia. It was the catalyst for the founding of the Colony of British Columbia, the building of early road infrastructure, and the founding of many towns.

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British Columbia Interior in the context of Kamloops, British Columbia

Kamloops (/ˈkæmlps/ KAM-loops) is a city in south-central British Columbia, Canada, at the confluence of the North and South Thompson Rivers, which join to become the Thompson River in Kamloops, and east of Kamloops Lake. The city is the administrative centre for, and largest city in, the Thompson-Nicola Regional District, a region of the British Columbia Interior.

The city was incorporated in 1893 with about 500 residents. The Canadian Pacific Railway was completed through downtown in 1886, and the Canadian National arrived in 1912, making Kamloops an important transportation hub. Kamloops North station is the first stop on VIA Rail's eastbound transcontinental service, The Canadian, while the Rocky Mountaineer and the Kamloops Heritage Railway both use Kamloops station.

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British Columbia Interior in the context of Quesnel Highland

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 boundary of the Quesnel Highland is not precisely defined in Holland, and in some interpretations it may be considered to be part of the Interior Plateau, as Holland defines it, or as a subrange of the Cariboo Mountains. Those mountains also, in some reckonings, are classified as part of the Interior Plateau rather than their usual association as the northernmost subrange of the Columbia Mountains. Generally it is composed of the lower, westerly valleys of Horsefly Lake, Quesnel Lake, and the Bowron Lakes, most of the Cariboo goldfield towns and similar terrain northwestwards, to about where the Willow River rounds the northern end of the Cariboo Mountains to join the Fraser River.

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British Columbia Interior in the context of Salmon Arm

50°42′8″N 119°16′20″W / 50.70222°N 119.27222°W / 50.70222; -119.27222Salmon Arm is a city in the Columbia Shuswap Regional District of the Southern Interior of the Canadian province of British Columbia that has a population of 19,432 (2021). Salmon Arm was incorporated as a municipal district on May 15, 2005. The city of Salmon Arm separated from the district in 1912, but was downgraded to a village in 1958. The city of Salmon Arm once again reunited with the District Municipality in 1970. Salmon Arm once again became a city in 2005, and is now the location of the head offices of the Columbia-Shuswap Regional District. It is a tourist town in the summer, connected to all 4 arms of Shuswap Lake, with many beaches, numerous golf courses, camping facilities, and house boat rentals. Salmon Arm is home to the longest wooden freshwater wharf in North America.

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British Columbia Interior in the context of Internment of Japanese Canadians

From 1942 to 1949, Canada forcibly relocated and incarcerated over 22,000 Japanese Canadians—comprising over 90% of the total Japanese Canadian population—from British Columbia in the name of "national security". The majority were Canadian citizens by birth and were targeted based on their ancestry. This decision followed the events of the Empire of Japan's war in the Pacific against the Western Allies, such as the invasion of Hong Kong, the attack on Pearl Harbor in Hawaii, and the Fall of Singapore which led to the Canadian declaration of war on Japan during World War II. Similar to the actions taken against Japanese Americans in neighbouring United States, this forced relocation subjected many Japanese Canadians to government-enforced curfews and interrogations, job and property losses, and forced repatriation to Japan.

From shortly after the December 1941 attack on Pearl Harbor until 1949, Japanese Canadians were stripped of their homes and businesses, then sent to internment camps and farms in British Columbia as well as in some other parts of Canada, mostly towards the interior. The internment in Canada included the theft, seizure, and sale of property belonging to this forcefully displaced population, which included fishing boats, motor vehicles, houses, farms, businesses, and personal belongings. Japanese Canadians were forced to use the proceeds of forced sales to pay for their basic needs during the internment.

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British Columbia Interior in the context of Carrier language

The Dakelh (ᑕᗸᒡ) or Carrier language is a Northern Athabaskan language. It is named after the Dakelh people, a First Nations people of the Central Interior of British Columbia, Canada, for whom Carrier has been a common English name derived from French explorers naming of the people. Dakelh people speak two related languages. One, Babine-Witsuwit'en, is sometimes referred to as Northern Carrier. The other includes what are sometimes referred to as Central Carrier and Southern Carrier.

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British Columbia Interior in the context of Hart Ranges

The Hart Ranges are a major subrange of the Canadian Rockies located in northeastern British Columbia and western Alberta. The mountains constitute the southernmost portion of the Northern Rocky Mountains.

The Hart Ranges were named in honour of British Columbia Premier John Hart, as is the highway which traverses the Pine Pass in the northern part of the range, connecting the north-central Interior of the province to the Peace River Regional District to the northeast.

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British Columbia Interior in the context of Gitxsan

Gitxsan (also spelled Gitksan and Kitksan) are an Indigenous people in Canada whose home territory comprises most of the area known as the Skeena Country in English (Git: means "people of" and Xsan: means "the River of Mist"). Gitksan territory encompasses approximately 35,000 km (14,000 sq mi) of land, from the basin of the upper Skeena River from about Legate Creek to the Skeena's headwaters and its surrounding tributaries. Part of the Tsimshianic language group, their culture is considered to be part of the civilization of the Indigenous peoples of the Pacific Northwest Coast, although their territory lies in the Interior rather than on the Coast. They were at one time also known as the Interior Tsimshian, a term which also included the Nisga'a, the Gitxsan's neighbours to the north. Their neighbours to the west are the Tsimshian (a.k.a. the Coast Tsimshian) while to the east the Wetʼsuwetʼen, an Athapaskan people, with whom they have a long and deep relationship and shared political and cultural community.

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