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.
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👉 Fraser Canyon in the context of Fraser Valley
The Fraser Valley is a geographical region in southwestern British Columbia, Canada and northwestern Washington State. It starts just west of Hope in a narrow valley encompassing the Fraser River and ends at the Pacific Ocean stretching from the North Shore Mountains, opposite the city of Vancouver BC, to just south of Bellingham, Washington.
In casual usage it typically describes the Fraser River basin downstream of the Fraser Canyon. The term is sometimes used outside British Columbia to refer to the entire Fraser River sections including the Fraser Canyon and up from there to its headwaters, but in general British Columbian usage the term refers to the stretch of Lower Mainland west of the Coquihalla River mouth at the inland town of Hope, and includes all of the Canadian portion of the Fraser Lowland as well as the valleys and upland areas flanking it. It is divided into the Upper Fraser Valley and Lower Fraser Valley by the Vedder River mouth at the eastern foothills of Sumas Mountain, although the Lower Valley section upstream of McMillan Island and the Salmon River mouth (at Fort Langley) used to be called the Central Fraser Valley up until 1995 (see Central Fraser Valley Regional District).
In this Dossier
- ⭐ Core Definition: Fraser Canyon
- 👉 Fraser Canyon in the context of Fraser Valley
- Fraser Canyon in the context of Fraser Canyon Gold Rush
- Fraser Canyon in the context of North Cascades
- Fraser Canyon in the context of Pasayten Wilderness
- Fraser Canyon in the context of Halkomelem
- Fraser Canyon in the context of Hope, British Columbia
Fraser Canyon 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.
Fraser Canyon in the context of North Cascades
The North Cascades are a section of the Cascade Range of western North America. They span the border between the Canadian province of British Columbia and the U.S. state of Washington and are officially named in the U.S. and Canada as the Cascade Mountains. The portion in Canada is known to Americans as the Canadian Cascades, a designation that also includes the mountains above the east bank of the Fraser Canyon as far north as the town of Lytton, at the confluence of the Thompson and Fraser Rivers.
They are predominantly non-volcanic, but include the stratovolcanoes Mount Baker, Glacier Peak and Coquihalla Mountain, which are part of the Cascade Volcanic Arc.
Fraser Canyon in the context of Pasayten Wilderness
The Pasayten Wilderness is a 531,539 acres (215,106 ha) protected area located within Okanogan–Wenatchee National Forest and Mount Baker National Forest in Washington state, centered on the Three Forks (48°54′02″N 120°38′01″W / 48.900584°N 120.6336808°W) of the Pasayten River, a tributary of the Similkameen River. Although part of the wilderness lies in Mount Baker-Snoqualmie National Forest, the largest section falls within the boundaries of Okanogan National Forest, which has responsibility for the wilderness's management. The wilderness is bordered by the Stephen Mather Wilderness to the west. The northern boundary of the wilderness is the Canada–US border. Across the border are Manning Provincial Park and Cathedral Provincial Park. The wilderness area is adjacent to the Ross Lake National Recreation Area to the west, and North Cascades National Park beyond that. The Pacific Crest National Scenic Trail has its northernmost section in this wilderness. The western part of the wilderness features dramatic views and peaks of the northern Washington Cascade Mountains while the eastern section is known for its grasslands and Alpine tundra. The tallest point in the Pasayten is Jack Mountain.
The Pasayten is traditional hunting territory of the Nlaka'pamux peoples of the Fraser Canyon and Nicola Country along with adjoining parts of the Cascade Range, although there are no Nlaka'pamux populations on the Washington side of the border.
Fraser Canyon in the context of Halkomelem
Halkomelem (/ˌhɒlkəˈmeɪləm/ HALL-kə-MAY-ləm; Halq̓eméylem in the Upriver dialect, Hul̓q̓umín̓um̓ in the Island dialect, and hən̓q̓əmin̓əm̓ in the Downriver dialect) is a language of various First Nations peoples of the British Columbia Coast. It is spoken in what is now British Columbia, ranging from southeastern Vancouver Island from the west shore of Saanich Inlet northward beyond Gabriola Island and Nanaimo to Nanoose Bay and including the Lower Mainland from the Fraser River Delta upriver to Harrison Lake and the lower boundary of the Fraser Canyon.
In the classification of Salishan languages, Halkomelem is a member of the Central Salish branch. There are four other branches of the family: Tsamosan, Interior Salish, Bella Coola, and Tillamook. Speakers of the Central and Tsamosan languages are often identified in ethnographic literature as "Coast Salish".
Fraser Canyon in the context of Hope, British Columbia
Hope is a district municipality at the confluence of the Fraser and Coquihalla rivers in the province of British Columbia, Canada. Hope is at the eastern end of both the Fraser Valley and the Lower Mainland region, and is at the southern end of the Fraser Canyon. To the east, over the Cascade Mountains, is the Interior region, beginning with the Similkameen Country on the farther side of the Allison Pass in Manning Park.Located 154 kilometres (96 mi) east of Vancouver, Hope is at the southern terminus of the Coquihalla Highway and the western terminus of the Crowsnest Highway, locally known as the Hope-Princeton (Highways 5 and 3, respectively), where they merge with the Trans-Canada Highway (Highway 1). Hope is at the eastern terminus of Highway 7. As it lies at the eastern end of the Fraser Valley in the windward Cascade foothills, the town gets very high amounts of rain and cloud cover – particularly throughout the autumn and winter.
Hope is a member municipality of the Fraser Valley Regional District which provides certain municipal services to unincorporated settlements and rural areas.