Lillooet, formerly Cayoosh Flat, is a community on the Fraser River in British Columbia, Canada, about 240 km (150 mi) up the British Columbia Railway line from Vancouver. Situated at an intersection of deep gorges in the lee of the Coast Mountains, it has a dry climate with an average of 329.5 mm (12.97 in) of precipitation being recorded annually. Lillooet has a long growing season, and once had prolific market gardens and orchard produce. It often vies with Lytton and Osoyoos for the title of "Canada's Hot Spot" on a daily basis in summer.
The Squamish-Lillooet Regional District is a quasi-municipal administrative area in British Columbia, Canada. It stretches from Britannia Beach in the south to Pavilion in the north. Lillooet, Pemberton, Whistler and Squamish are the four municipalities in the regional district. Its administrative offices are in the Village of Pemberton, although the district municipalities of Squamish, Whistler, and Lillooet are all larger population centres. The district covers 16,353.68 km² of land area.
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, British Columbia at Soda Creek Canyon near the town of the same name.
Shalalth, pop. c. 400, is one of the main communities of the Seton Lake Band of the St'at'imc (Lillooet) Nation and location of the two main powerhouses of the Bridge River Power Project.
The Cariboo Gold Rush was a gold rush in the Colony of British Columbia, which later joined 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 Lillooet River is a major river of the southern Coast Mountains of British Columbia. It begins at Silt Lake, on the southern edge of the Lillooet Crown Icecap about 80 kilometres northwest of Pemberton and about 85 kilometres northwest of Whistler. Its upper valley is about 95 kilometres in length, entering Lillooet Lake about 15 km downstream from Pemberton on the eastern outskirts of the Mount Currie reserve of the Lil'wat branch of the St'at'imc people. From Pemberton Meadows, about 40 km upstream from Pemberton, to Lillooet Lake, the flat bottomlands of the river form the Pemberton Valley farming region.
The Douglas Road, a.k.a. the Lillooet Trail, Harrison Trail or Lakes Route, was a goldrush-era transportation route from the British Columbia Coast to the Interior. Over 30,000 men are reckoned to have travelled the route in, although by the end of the 1860s it was virtually abandoned due to the construction of the Cariboo Wagon Road, which bypassed the region.
Anderson Lake is located about 25 miles North of the town of Pemberton, British Columbia and is about 28.5 km2 in area and around 21 km (13 mi) in length. Its maximum depth is 215 meters. It is drained by the Seton River, which feeds Seton Lake and so the Fraser River. It is fed by the Gates River, which drains from the Pemberton Pass divide with the Birkenhead River valley towards Pemberton-Mount Currie.
The Cayoosh Gold Rush was one of several in the history of the region surrounding Lillooet, British Columbia, Canada. If estimates of its yield are true, it would be one of the richest single finds in the gold mining history of that province.
N'Quatqua, variously spelled Nequatque, N'quat'qua, is the proper historic name in the St'at'imcets language for the First Nations village of the Stl'atl'imx people of the community of D'Arcy, which is at the upper end of Anderson Lake about 35 miles southeast of Lillooet and about the same distance from Pemberton. The usage is synonymous with Nequatque Indian Reserve No. 1, which is 177 ha. in size and located adjacent to the mouth of the Gates River.
Pemberton is a village municipality north of Whistler in the Pemberton Valley of British Columbia in Canada, with a population of 2,574. Until the 1960s the village could be reached only by train, but that changed when Highway 99 was built through Whistler and Pemberton.
Gold Bridge is an unincorporated community in the Bridge River Country of British Columbia, Canada. Although numbering only around 40 inhabitants, Gold Bridge is the service and supply centre for the upper basin of the Bridge River Valley, which includes recreation-residential areas at the Gun Lakes, Tyaughton Lake, Marshall Creek, and Bralorne; and the nearby ghost towns of Brexton and Pioneer Mine.
The Sea-to-Sky Corridor, often referred to as the Corridor or the Sea to Sky Country, is a region in British Columbia spreading from Horseshoe Bay through Whistler to the Pemberton Valley and sometimes beyond to include Birken and D'Arcy. From Whistler on up, the region overlaps with the older and more historic Lillooet Country, of which Squamish, at the region's centre, was once the southward extension in the days when it was the rail-port terminus from the Interior, via Lillooet, and accessible from the Lower Mainland only by sea. Most of the region is in the Squamish-Lillooet Regional District, although south of Britannia Beach a small part of the region is in the Greater Vancouver Regional District.
D'Arcy is an unincorporated community in the Canadian province of British Columbia, approximately 150 kilometres northeast of the city of Vancouver. Located at the head of Anderson Lake, D'Arcy, also known as Nequatque or N'Quatqua in the St'at'imcets (Lillooet) language, is partly a recreational and resource community and also the territory and residential area of the N'Quatqua First Nation.
The Lil'wat First Nation, a.k.a. the Lil'wat Nation or the Mount Currie Indian Band, is a First Nation band government located in the southern Coast Mountains region of the Interior of the Canadian province of British Columbia. It is a member of the Lillooet Tribal Council, which is the largest grouping of band governments of the St'at'imc or Stl'atl'imx people. Other St'at'imc governments include the smaller In-SHUCK-ch Nation on the lower Lillooet River to the southwest, and the independent N'quatqua First Nation at the near end of Anderson Lake from Mount Currie, which is the main reserve of the Lil'wat First Nation, and also one of the largest Indian reserves by population in Canada.
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,.
Pemberton Pass, 505 m (1,657 ft), also formerly known as Mosquito Pass, is the lowest point on the divide between the Lillooet and Fraser River drainages, located at Birken, British Columbia, Canada, in the principal valley connecting and between Pemberton and Lillooet. The pass is a steep-sided but flat-bottomed valley adjacent to Mount Birkenhead and forming a divide between Poole Creek, a tributary of the Birkenhead River, which joins the Lillooet at Lillooet Lake, and the Gates River which flows northeast from Gates Lake, at the summit of the pass, which flows to the Fraser via Anderson and Seton Lakes and the Seton River.
Birken is an unincorporated community, located at Gates Lake in the Gates Valley of the Lillooet Country in the Southern Interior of British Columbia, Canada, approximately midway in the route known as the Long Portage or Pemberton Pass, which connects the Pemberton Valley to the Fraser Canyon via Anderson and Seton Lakes via the Seton River. Birken, and Birken Lake, are at the summit of that pass, which was part of the important Fraser Canyon Gold Rush-era route known as the Douglas Road.
Cayoosh Creek is a northeast-flowing tributary of the Seton River in the Canadian province of British Columbia. The name Cayoosh Creek remains on the bridge-sign crossing the stream on BC Highway 99 and continues in use locally to refer to the final reaches of the Seton River, formerly Seton Creek, which prior to the renaming ending at the confluence with Cayoosh Creek. The creek is the namesake of Cayoosh Creek Indian Reserve No. 1, one of the main Indian reserves of the Cayoose Creek Indian Band, which lies adjacent to what was renamed the Seton River without local consultation.
Canada 
British Columbia