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Nation Lakes

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The Nation Lakes are a series of four lakes in the Nation River system of the Omineca Country of the Central Interior of British Columbia , Canada . The four lakes are, from west to east (downstream), Tsayta , Indata , Tchentlo , and Chuchi Lakes . Nation Lakes Park was established in 2004 as a result of the Fort St. James Land Resource Management Plan and is a popular canoeing destination.

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26-511: 55°12′00″N 124°45′00″W  /  55.20000°N 124.75000°W  / 55.20000; -124.75000 This article about a location in the Interior of British Columbia , Canada is a stub . You can help Misplaced Pages by expanding it . British Columbia Interior The British Columbia Interior , popularly referred to as the BC Interior or simply the Interior ,

52-510: A few cases that is also a phrase referring to the land district of the same name, which is a system of legal survey blocks rather than descriptive of the actual geocultural landscape which evolved on top of them. In most cases, the "Country" and "District" are often dropped, and these regions are referred to as, for example, "the Kootenay" or "the Omineca". In some cases, notably the Kootenay,

78-475: A short freeway. Then it continues 496 km (308 mi) east through Salmon Arm , Revelstoke , Rogers Pass , Golden , and Kicking Horse Pass (the highest point on the highway, at 1,627 metres), to Banff , Alberta. Cariboo The Cariboo is an intermontane region of British Columbia , Canada, centered on a plateau stretching from Fraser Canyon to the Cariboo Mountains . The name

104-666: 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

130-468: Is a reference to the caribou that were once abundant in the region. The Cariboo was the first region of the interior north of the lower Fraser River and its canyon to be settled by non-indigenous people, and played an important part in the early history of the colony and province. The boundaries of the Cariboo proper in its historical sense are debatable, but its original meaning was the region north of

156-596: Is incorrect. The Southern Interior roughly falls south of the Thompson River and Shuswap Country (corresponding mostly to the post- Oregon Treaty remainder of the old, original, Hudson's Bay Company Columbia District ). When used directly, it generally means the Okanagan and adjoining areas, particularly the Similkameen , southern Monashees and Boundary Country . Due to a new federal political riding of

182-679: Is often broken up informally as the Northern Interior, the Central Interior, the Southern Interior, the Northeast Interior and Southeast Interior, and these names often appear in non-governmental organizations and company names as well as in government administrative districts and ministerial regions, and in weather reports. Below are the 14 regional districts of British Columbia defined as being in

208-722: The Rocky Mountains and, in the northeast, British Columbia's sector of the Prairies, the Peace River Block . "Interior" is usually and properly capitalized but turns up in lower-case in various books and magazines. The non-coastal areas of the province are considered to be "in the Interior", although the sparsely populated regions of its northern half are usually referred to only as "the North". The town of Hope , at

234-943: The Chilcotin and the Cariboo, they can be are often referred to as simply Kootenay, Chilcotin and Cariboo.. Some are referred to only without the "Country" or "District" attached, such as "the Tulameen" and "the Similkameen", and in other cases this is more common than the longer form though both occur ("the Stikine" is more common than "the Stikine Country". Combination forms are common, such as Cariboo-Chilcotin, and Thompson-Okanagan, and these often turn up in names of governmental administrative districts, electoral districts and private or public organizations. All often correspond to linguistic and cultural-political divisions of

260-474: The First Nations as aboriginal history was also shaped by the landscape's isolating and defining characteristics as settler culture. The main historical subregions, with their own subregions an irrespective of very common overlaps between some areas, and in their most common forms, are as follows: As of 2016 the population is 961,155. The British Columbia Interior's society and culture is affected by

286-707: The Fraser basin) to the southeast of Prince George as well as the Omineca District and the Bulkley and Nechako basins. The communities of the upper Skeena are sometimes referred to as being in the Northern Interior, though in cultural terms and usual usage they are part of the North Coast , which is associated in regional terms usually with the South and Central Coast and Vancouver Island. The northern reaches of

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312-571: The Highway 99 corridor is nominally between Whistler and Pemberton , as Pemberton is often described as being in the Interior, but from the inland perspective it is often seen as part of the Coast because of its wetter climate and close ties to the Lower Mainland. There are many subregions within the Interior, some regions in their own right, and although there are no precise definitions, it

338-517: The Interior region: The Northern Interior begins somewhere between the Cariboo and the city of Prince George , which lies just south of the big bend in the upper Fraser. The city of Quesnel may be considered to be part of the Northern Interior, but it is usually conceived of as primarily being in the Cariboo, which is normally termed the Central Interior, or North-Central Interior. The Northern Interior includes Robson Valley (the upper reaches of

364-708: The Lillooet Country is historically considered to be part of the Cariboo, though distinct in its own right. The Bridge River Country has also been referred to as the West Cariboo, but is not considered to be in the Cariboo by its residents. Many urban residents are under the impression that the Bridge River Country is part of the Chilcotin because of the "South Chilcotin" name for the Spruce Lake Protected Area , but this

390-548: The North". The Northern Interior Plain is a continuation of the interior plain that takes in nearly all of Alberta and southern Saskatchewan and Manitoba. It extends from Monkman Provincial Park and Tumbler Ridge in the south, to Hudson's Hope and the Williston Lake in the west, to Fort St. John and Charlie Lake in the north. The term is used to mean the whole of the Northeastern Interior east of

416-411: The Northern Interior beyond the Omineca and Skeena-Bulkley regions is usually just referred to as "the North", although it also is considered part of the Northern Interior . "The North" may also refer to Prince George, one of the largest cities in the Interior and also the only major city in the Northern Interior (although that term can also apply to Prince George), which bears the sobriquet "Queen City of

442-641: The Okanagan cities south of the Shuswap as being in the Central Interior, but these are usually referred to as being in the Southern Interior or South-Central Interior. The Nicola, Fraser Canyon, Thompson and Bridge River -Lillooet Country are sometimes also referred to as being in the Southern Interior, with the Bridge River-Lillooet Country sometimes referred to, along with the Chilcotin, as the West-Central Interior, and

468-562: The Rockies, including Fort Nelson and other parts of the Liard drainage , and before W.A.C. Bennett Dam included the upper Peace River through its canyon between Finlay Forks and Hudson's Hope. The Central Interior is composed, roughly, of the Chilcotin , Cariboo, Bridge River - Lillooet , Fraser Canyon, Nicola , Thompson and Kamloops - Shuswap Countries . Some usages may refer to

494-419: 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,

520-662: The eastern end of the Fraser Valley and at the foot of the Fraser Canyon , is often considered the "Gateway to the Interior" and bears an entrance arch to that effect, though in practical terms the Interior does not begin until somewhere between Yale and Boston Bar , in the Fraser Canyon, or until the summits of the Coquihalla and Allison Passes . The boundary between "the Coast" and "the Interior" along

546-659: The forks of the Quesnel River and the low mountainous basins between the mouth of that river on the Fraser at the city of Quesnel and the northward end of the Cariboo Mountains, an area that is mostly in the Quesnel Highland and focused on several now-famous gold-bearing creeks near the head of the Willow River . The richest of them all, Williams Creek , is the location of Barkerville , which

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572-548: The populations of First Nations Canadians and French-Canadians people and residents living close to the US - Canada border. The Trans-Canada Highway (TCH) is the major roadway through the region. The TCH enters the region from the south after 186 km (116 mi) through the Fraser Canyon in the Lower Mainland toward Cache Creek . As a mostly high mobility highway with only occasional mandatory stops, it heads east for 79 km (49 mi) through to Kamloops where it becomes

598-611: The province and well over 80% of its mainland. As it consists of a series of interlocking valleys and plateaus, geographic effects relating to isolation, physical remoteness, local indigenous culture, the background of various groups of settlers, and more, have contributed to an identifiable patchwork of regional identities, referred to as "districts" or "countries" (e.g., the Omineca Country, the Boundary Country). Usage such as "Lillooet District" are also common but in

624-530: 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. The region, which includes the Interior Plateau as well as various mountain ranges and the valleys between them, comprises everything inland from the Coast Mountains and reaching east to

650-852: The same name (see Southern Interior ) the usage has now come to apply to the cities of the West Kootenay , along with the rest of the Kootenays , although the West Kootenay has usually been referred to in the past, and is today, as the Southeast Interior. The Big Bend of the Columbia and the Rocky Mountain Trench are in the Interior, but are not usually included in mentions of either the Central Interior or Southern Interior. The Interior comprises over 70% of

676-553: Was both the capital of the Cariboo Gold Rush and of government officialdom for decades afterwards (it is now a museum town). The Cariboo goldfields are underpopulated today but were once the most settled and most significant of the regions of interior British Columbia. As settlement spread southwards of this area, flanking the route of the Cariboo Road and spreading out through the rolling plateaus and benchlands of

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