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Lillooet is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road about 100 kilometres (62 mi) northeast of Pemberton, 64 kilometres (40 mi) northwest of Lytton, and 172 kilometres (107 mi) west of Kamloops.
Lytton is a village of about 250 residents in southern British Columbia, Canada, on the east side of the Fraser River and primarily the south side of the Thompson River, where it flows southwesterly into the Fraser. The community includes the Village of Lytton and the surrounding community of the Lytton First Nation, whose name for the place is Camchin, also spelled Kumsheen.
Yale is an unincorporated town in the Canadian province of British Columbia, which grew in importance during the Fraser Canyon Gold Rush.
British Columbia gold rushes were important episodes in the history and settlement of European, Canadian and Chinese peoples in western Canada.
The Cariboo Road was a project initiated in 1860 by the Governor of the Colony of British Columbia, James Douglas. 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.
Yale-Lillooet was a provincial electoral district for the Legislative Assembly of 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.
The Cariboo Gold Rush was a gold rush in the Colony of British Columbia, which later became the Canadian province of British Columbia. The first gold discovery was made at Hills Bar in 1858, followed by more strikes in 1859 on the Horsefly River, and on Keithley Creek and Antler Creek in 1860. The actual rush did not begin until 1861, when these discoveries were widely publicized. By 1865, following the strikes along Williams Creek, the rush was in full swing.
The Fraser Canyon 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 centered on the Fraser Canyon from around Hope and Yale to Pavilion and Fountain, just north of Lillooet.
The Camelsfoot Range is a sub-range of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains in British Columbia. The Fraser River forms its eastern boundary. The range is approximately 90 km at its maximum length and less than 30 km wide at its widest.
The Okanagan Trail was an inland route to the Fraser Canyon Gold Rush from the Lower Columbia region of the Washington and Oregon Territories in 1858–1859. The route was essentially the same as that used by the Hudson's Bay Company fur brigades, following the Columbia River to the confluence of the Okanogan River, and then up that river's watercourse via Osoyoos, Skaha (Dog) and Okanagan lakes, then using a pass via Monte Creek to Fort Kamloops, at the confluence of the North and South Thompson rivers. From there, the route went west down the Thompson River either to the lower gold-bearing bars of the Fraser River between what is now Lytton, British Columbia and Yale, British Columbia, or via Hat Creek and Marble Canyon to the upper Fraser goldfields around present-day Lillooet, British Columbia. A shorter branch-route to the lower Thompson and lower Fraser Canyon diverged from the main route at the confluence of the Similkameen River and the Okanogan. Cayoosh and The Fountains are today's Lillooet, British Columbia and environs.
Soda Creek is a rural subdivision 38 km north of Williams Lake in British Columbia, Canada. Located on the east bank of the Fraser River, Soda Creek was originally the home of the Xat'sull First Nation. Soda Creek Indian Reserve No. 1 is located on the left (E) bank of the Fraser River, one mile south of the Soda Creek BCR (CN) station, 431.10 ha. 52°19′00″N122°16′00″W
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 Lytton First Nation, a First Nations band 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.
The River Trail was a main route for travel in the colonial era of what is now the Canadian province of British Columbia, running northwards along the Fraser River from to present day Lillooet to Big Bar, British Columbia and points beyond in the Cariboo District. The route was primarily in use during the Fraser Canyon Gold Rush and associated explorations by prospectors northwards in the search for gold in the Cariboo and Omineca Districts.
The Lillooet Country, also referred to as the Lillooet District, is a region spanning from the central Fraser Canyon town of Lillooet west to the valley of the Lillooet River, and including the valleys in between, in the Southern Interior of British Columbia. Like other historical BC regions, it is sometimes referred to simply as The Lillooet or even Lillooet,.
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.
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.
Fountain Valley, officially named Three Lake Valley and also known as the Fountain Lakes Valley, is a valley and rural community located on the east flank of Fountain Ridge, just east of the town of Lillooet, British Columbia, Canada and immediately south of the Indian reserve community of Fountain. The valley is historically significant as part of the River Trail, which ran up the length of the Fraser River from Yale to Big Bar and beyond, diverging at various points to connect to trails farther east and with the Old Cariboo Road at Fountain, then known as the Upper Fountains and an important junction and staging-ground for freight wagons and travellers bound northwards to the Cariboo goldfields. The trail through the valley, which developed into a wagon road whose roadgrade is largely used by today's road through the valley, climbs a steep grade from its southern end, near Fountainview Farms on the Fraser, and descends relatively gently towards Fountain. The three lakes in the valley, which give it its official name, are Cinquefoil Lake, Kwotlenemo Lake, and Chilhil Lake, the three of them collectively being known as the Fountain Lakes There are many recreational dwellings and small ranches forming a community in the valley, which is something of a rural "suburb" of Lillooet.
The Bridge River Rapids, also known as the Six Mile Rapids, the Lower Fountain, the Bridge River Fishing Grounds, and in the St'at'imcets language as Sat' or Setl, is a set of rapids on the Fraser River, located in the central Fraser Canyon at the mouth of the Bridge River six miles north of the confluence of Cayoosh Creek with the Fraser and on the northern outskirts of the District of Lillooet, British Columbia, Canada.
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