Related Research Articles
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 Stʼatʼimc, also known as the Lillooet, St̓át̓imc, Stl'atl'imx, etc., are an Interior Salish people located in the southern Coast Mountains and Fraser Canyon region of the Interior of the Canadian province of British Columbia.
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.
The Lillooet Ranges are the southeasternmost subdivision of the Pacific Ranges of the Coast Mountains of British Columbia. They are located between the drainage of the Lillooet River and Harrison Lake on the west and the canyon of the Fraser River on the east, and by the lowland coastal valley of that river on the south.
Harrison Lake is the largest lake in the southern Coast Mountains of Canada, being about 250 square kilometres (95 mi²) in area. It is about 60 km (37 mi) in length and at its widest almost 9 km (5.6 mi) across. Its southern end, at the resort community of Harrison Hot Springs, is c. 95 km east of downtown Vancouver. East of the lake are the Lillooet Ranges while to the west are the Douglas Ranges. The lake is the last of a series of large north-south glacial valleys tributary to the Fraser along its north bank east of Vancouver, British Columbia. The others to the west are the Chehalis, Stave, Alouette, Pitt, and Coquitlam Rivers.
Marble Canyon is in the south-central Interior of British Columbia, a few kilometres east of the Fraser River and the community of Pavilion, midway between the towns of Lillooet and Cache Creek. The canyon stems from a collapsed karst formation.
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.
A quiggly hole, also known as a pit-house or simply as a quiggly or kekuli, is the remains of an earth lodge built by the First Nations people of the Interior of British Columbia and the Columbia Plateau in the United States The word quiggly comes from kick willy or keekwulee, the Chinook Jargon word for "beneath" or "under".
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.
Thompson Country, also referred to as The Thompson and sometimes as the Thompson Valley and historically known as the Couteau Country or Couteau District, is a historic geographic region of the Southern Interior of British Columbia, more or less defined by the basin of the Thompson River. This is a tributary of the Fraser; the major city in the area is Kamloops.
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.
The Nahatlatch River is a tributary of the Fraser River in the Canadian province of British Columbia. It originates in the Lillooet Ranges of the Coast Mountains and empties into the Fraser River in the Fraser Canyon, north of Boston Bar.
Churn Creek is a tributary of the Fraser River in the Canadian province of British Columbia.
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.
Pavilion Mountain is a mountain in the Marble Range in the South Cariboo region of the South-Central Interior of British Columbia, Canada, located northeast of the ranching and First Nations community of Pavilion and to the north of Marble Canyon and immediately south of Kelly Lake, which is the focus of Downing Provincial Park. The term Pavilion Mountain is also used to refer to the historic ranch and associated rangeland on the "bench" on the mountain's southwestern side, and also to the road which traverses that benchland and the mountain's western shoulder and is the route of the Old Cariboo Road. The switchback descent from the summit of the road was known as the Rattlesnake Grade and was an infamous stretch of the old wagon road. From a junction at the road-summit, a road leads east along the spine of the mountain to the peak, which is the site of a microwave relay and former fire lookout. The mountain's only named subpeak, Mount Carson, at 2005 metres, is southeast of the fire lookout and is named for the original owner of the ranch and was briefly misapplied as the name of Pavilion Mountain. Robert Carson was one of the first settlers in the region and whose sons later became prominent MLAs and provincial cabinet ministers. The north wall of Marble Canyon is essentially the southeast buttress of Pavilion Mountain.
Mission Ridge, also known as Mission Mountain, is a ridge in the Bridge River-Lillooet Country of the South-Central Interior of British Columbia, Canada, extending westward from the town of Lillooet along the north side of Seton Lake to Mission Pass, which is immediately above and to the north of the lakeside community of Shalalth. The road over the pass is also known as Mission Mountain, which is short for "Mission Mountain Road". Mission Creek lies on the north side of the pass, and is a tributary of the Bridge River, the lower reaches of which lie on the north side of the ridge, and which was the only road access into the upper Bridge River Country before the construction of a road through the Bridge River Canyon in the mid-1950s opened that region up to road access from the lower Bridge River valley and the town of Lillooet via the community or Moha. Most, or virtually all, of the ridge, is Indian Reserves, notably Slosh 1, under the administration of the Seton Lake Indian Band, and Bridge River 1, which is under the administration of the Bridge River Indian Band. Parts of the ridge's eastern end are in reserves controlled by the Lillooet Indian Band, including its final spires above Lillooet, which were dubbed St. Mary's Mount by the Reverend Lundin Brown in the 1860s, though that name never stuck and is ungazetted.
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.
Keatley Creek is a significant archaeological site in the interior of British Columbia and in the traditional territory of the St'at'imc peoples. Its location is in the Glen Fraser area of the Fraser Canyon ranchlands about 18 miles from the town of Lillooet on a benchland flanking Keatley Creek, whose name derives from a former ranch owner, and from which the site takes its name.
Texas Creek is a medium-sized right tributary of the Fraser River in the Fraser Canyon region of that river's course, located approximately 16 miles down the river from the town of Lillooet. Texas Creek is also the name of the rural neighbourhood in the area of the creek, and also that of the Texas Creek Ranch which is one of the larger holdings.
Glen Fraser is a locality in the central Fraser Canyon of the Central Interior of British Columbia, Canada, located c. 18 miles north of the town of Lillooet and between the communities of Fountain (S) and Pavilion. It is a ranching area formed of benchlands on the west side of the Fraser and is the location of the Keatley Creek Archaeological Site, one of Canada's most important ongoing investigations. The name was conferred as that of a railway stop on the Pacific Great Eastern Railway, now Canadian National.
References
Coordinates: 50°47′50″N121°51′30″W / 50.79722°N 121.85833°W