Pemberton Valley

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The Pemberton Valley is a valley flanking the Lillooet River upstream from Lillooet Lake, including the communities of Mount Currie, Pemberton, British Columbia and the agricultural district surrounding them and flanking the river as far upstream as the Pemberton Meadows area. The term is normally used only to refer to inhabited parts of the valley, not the unsettled areas to the north of Pemberton Meadows although the official definition extends from the head of Lillooet Lake all the way up to the confluence of Meager Creek. Historically the region was part of the Lillooet Country but due to re-orientation of the area's economy and society since the opening and expansion of BC Highway 99 the area is now more considered to be part of the Sea-to-Sky Corridor.

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<span class="mw-page-title-main">Squamish-Lillooet Regional District</span> Regional district in British Columbia, Canada

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 and Whistler are larger population centres. The district covers 16,353.68 km² of land area.

The Skatin First Nations, aka the Skatin Nations, are a band government of the In-SHUCK-ch Nation, a small group of the larger St'at'imc people who are also referred to as Lower Stl'atl'imx. The Town of Skatin - the St'at'imcets version of the Chinook Jargon Skookumchuck- is located 4 km south of T'sek Hot Spring- alt. spelling T'sek Hot Spring - commonly & formerly named both St. Agnes' Well & Skookumchuck Hot Springs The community is 28 km south of the outlet of Lillooet Lake on the east side of the Lillooet River. It is approximately 75 km south of the town of Pemberton and the large reserve of the Lil'wat branch of the St'at'imc at Mount Currie. Other bands nearby are Samahquam at Baptiste Smith IR on the west side of the Lillooet River at 30 km. and Xa'xtsa First Nations; the latter is located at Port Douglas, near the mouth of the Lillooet River where it enters the head of Harrison Lake. The N'Quatqua First Nation on Anderson Lake, between Mount Currie and Lillooet, was at one time involved in joint treaty negotiations with the In-SHUCK-ch but its members have voted to withdraw, though a tribal council including the In-SHUCK-ch bands and N'Quatqua remains, the Lower Stl'atl'imx Tribal Council.

<span class="mw-page-title-main">Lillooet River</span> River in British Columbia, Canada

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.

<span class="mw-page-title-main">Cayoosh Range</span>

The Cayoosh Range is the northernmost section of the Lillooet Ranges, which are a subrange of the Pacific Ranges of the Coast Mountains in British Columbia, Canada. The range covers an area of c. 3770 km² and is approximately 65 km (40 mi) SW to NE and about 20 km (12 mi) SE to NW.

<span class="mw-page-title-main">Birkenhead River</span>

The Birkenhead River, formerly known as the Portage River, the Pole River and the Mosquito River, is a major tributary of the Lillooet River, which via Harrison Lake and the Harrison River is one of the major tributaries of the lower Fraser River. It is just over 50 km long from its upper reaches in the unnamed ranges south of Bralorne, British Columbia ; their western area towards the named Bendor Range east of Bralorne is sometimes called the Cadwallader Ranges.

<span class="mw-page-title-main">Birkenhead Lake Provincial Park</span> Provincial park

Birkenhead Lake Provincial Park is a provincial park in British Columbia, Canada, located in the Lillooet Country region to the northeast of Pemberton and immediately northwest of Birkenhead Peak and Gates Lake at the community of Birken.

<span class="mw-page-title-main">Stswecem'c Xgat'tem First Nation</span> First Nation government in British Columbia, Canada

The Stswecem'c Xgat'tem First Nation, formerly known as Canoe Creek Band/Dog Creek Indian Band, created as a result of merger of the Canoe Creek Band and Dog Creek Band is a First Nations government of the Secwepemc (Shuswap) Nation, located in the Fraser Canyon-Cariboo region of the Central Interior of the Canadian province of British Columbia. It was created when the government of the then-Colony of British Columbia established an Indian reserve system in the 1860s. It is a member government of the Northern Shuswap Tribal Council.

The Tl'etinqox-t'in Government Office is a First Nations government located in the Chilcotin District in the western Central Interior region of the Canadian province of British Columbia. Governing a reserve communities near Alexis Creek known as Anaham Reserve First Nations or Anaham, it is a member of the Tsilhqot'in Tribal Council aka known as the Tsilhqot'in National Government. The main reserve is officially known as Anahim's Flat No. 1, and is more commonly as Anaham. Other reserves are Anahim's Meadow No. 2 and 2A, and Anahim Indian Reserves Nos. 3 through 18. Anaham, or Anahim and Alexis were chiefs of the Tsilhqot'in during the Chilcotin War of 1864, although they and their people did not take part in the hostilities.

<span class="mw-page-title-main">Lil'wat First Nation</span> First Nation band government

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 Icecap, also called the Lillooet Icefield or the Lillooet Crown, is a large icefield in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is about 90 km (56 mi) northwest of the towns of Pemberton and Whistler, and about 175 km (109 mi) north of Vancouver, British Columbia. The Lillooet Icecap is one of the largest of several large icefields in the Pacific Ranges which are the largest temperate-latitude glacial fields in the world. At its maximum extent including its glacial tongues it measures 30 km (19 mi) east to west and 20 km (12 mi) north to south; its central icefield area is approximately 15 km (9 mi) in diameter.

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.

Railroad Pass, 1385 m (4544 ft), usually known locally as Railway Pass, is a mountain pass in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Traversed by a seasonal dirt road known as the Hurley Main and sometimes also referred to therefore as Hurley Pass, the pass connects the Pemberton Meadows area of the upper valley of the Lillooet River, via Railroad Creek, to the uppermost reaches of the Hurley River, the main south fork of the Bridge River which the Hurley joins at the settlement of Gold Bridge.

The Nazko First Nation is a First Nations government of the Dakelh people in the north-central Interior of British Columbia. Its reserves are located around the community of Nazko, British Columbia, which is 120 km west of Quesnel and southwest of Prince George.

The Pemberton Icefield or Pemberton Icecap, is the southernmost of the series of very large icefields studding the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada.

The Dewdney-Alouette Regional District was a regional district in the Lower Mainland of British Columbia, Canada, comprising the district municipalities of Pitt Meadows, Maple Ridge and Mission and unincorporated areas east to the Harrison River and north to the southern end of Lillooet Lake. The regional district was partitioned when the Greater Vancouver Regional District was expanded in 1995 to take in Pitt Meadows and Maple Ridge; the regional district's eastern half was combined with the former Central Fraser Valley Regional District and the Regional District of Fraser-Cheam to form the Fraser Valley Regional District.

The Gates Valley is a valley and group of communities in the Lillooet Country of the Southern Interior of British Columbia, Canada, located between the summit of Pemberton Pass and the head of Anderson Lake at the community of D'Arcy. Though the term strictly refers to the valley of the Gates River, it is usually used more in a sense of the communities located in the valley and is not a term used for the river's drainage basin, which is much larger.

<span class="mw-page-title-main">Rocky Mountain Foothills</span> Upland area in western Canada

The Rocky Mountain Foothills are an upland area flanking the eastern side of the Rocky Mountains, extending south from the Liard River into Alberta. Bordering the Interior Plains system, they are part of the Rocky Mountain System or Eastern System of the Western Cordillera of North America.

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The Lillooet Land District is one of the 59 cadastral subdivisions of British Columbia, which were created by the Lands Act of the Colony of British Columbia in 1859, defined as "a territorial division with legally defined boundaries for administrative purposes". The land district's boundaries came to be used as the boundary of the initial Lillooet riding for the provincial Legislature from 1871, when the colony became a province. In addition to use in descriptions of land titles and lot surveys, the Land District was also the basis of the Lillooet Mining District.

The Cariboo Land District is a cadastral survey subdivision of the province of British Columbia, Canada, created with rest of those on Mainland British Columbia via the Lands Act of the Colony of British Columbia in 1860. The British Columbia government's BC Names system, a subdivision of GeoBC, defines a land district as "a territorial division with legally defined boundaries for administrative purposes" All land titles and surveys use the Land District system as the primary point of reference, and entries in BC Names for placenames and geographical objects are so listed.

References

Coordinates: 50°30′00″N123°00′00″W / 50.50000°N 123.00000°W / 50.50000; -123.00000