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". [1] 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.
Included in the Land District are the historical region known as the Lillooet Country, including the Pemberton Valley, and the southeast Chilcotin and South Cariboo areas. Major landforms in the land district include the Pemberton Icecap and the Lillooet Icecap.
Municipalities within the land district are Pemberton, Lillooet, 100 Mile House and Clinton. Other communities include D'Arcy, Shalalth, Seton Portage, Fountain, Pavilion, Gold Bridge, Bralorne, Jesmond, and 70 Mile House.
To the south, the Lillooet Land District borders with the New Westminster Land District, on the west with the Sayward Land District and Coast Land District Range 1, on the north with the Cariboo Land District, and on the east and southeast, the Kamloops Division, Yale Land District.
Starting at a point just north of the head of Jervis Inlet, at 50 degrees 13 minutes north latitude, 124 degrees west longitude, north to 52 degrees north latitude, 124 degrees west longitude, then, with some small deviances south around parcels of land that are part of the Cariboo Land District east along the 52nd parallel north to approximately 120 degrees, 33 minutes west longitude, crossing BC Hwy 97 at the Begbie Summit. From there, south along that longitude, passing between Canim Lake and Mahood Lake, bisecting Bonaparte Lake, to 51 degrees 2 minutes north latitude, just northwest of Silwhoiakun Mountain, then west to 51 degrees 4 minutes latitude, between Loon Lake (British Columbia) and Hihium Lake, with deviances north and south around parcels of land. From there, the boundary follows land parcel boundaries in a jagged curving line to 50 degrees 45 minutes north latitude at 121 degrees 46 west longitude, just northwest of the summit of Chipuin Mountain, to 50 degrees 34 121 degrees 45 west. From there, via another jagged arc around land to cross the Fraser in the area of Fountainview Farm and Foster Bar to 50 degrees 31 minutes north latitude at 121 degrees 48 minutes west longitude. From that point the boundary follows the divide between the Cayoosh Creek and Stein River basins, and that between the Stein basin and that of the Lillooet River, to a point at the western end of the icefields on the Mount Skook Jim massif at 50 degrees 7 minutes north, 122 degrees 15 minutes west, then west, crossing the Lillooet River drainage between Lillooet Lake and Little Lillooet Lake to 50 degrees 7 minutes north, 122 38 degrees west, and following the mountain ridges to 50 degrees 14 minutes north at 122 degrees 45 minutes west, just southwest of the summit of Mount Currie. West along that latitude, the boundary deviates south slightly in the area of the Soo Valley such that surveys in that area are in the Lillooet Land District, and then continues west to the point just north of the head of Jervis Inlet. [2]
Lillooet is a town in the Fraser Canyon in British Columbia.
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.
Cariboo was a federal electoral district in British Columbia, Canada, that was represented in the House of Commons of Canada from 1871 to 1892.
The Pacific Ranges are the southernmost subdivision of the Coast Mountains portion of the Pacific Cordillera. Located entirely within British Columbia, Canada, they run northwest from the lower stretches of the Fraser River to Bella Coola and Burke Channel, north of which are the Kitimat Ranges. The Coast Mountains lie between the Interior Plateau and the Coast of British Columbia.
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.
Cariboo was one of the twelve original electoral districts created when British Columbia became a Canadian province in 1871. Roughly corresponding to the old colonial electoral administrative district of the same name, it was a three-member riding until the 1894 election, when it was reduced through reapportionment and became a two-member riding until the 1916 election, after which it has been a single-member riding. It produced many notable Members of the Legislative Assembly (MLAs), including George Anthony Boomer Walkem, third and fifth holder of the office of Premier of British Columbia and who was one of the first representatives elected from the riding; John Robson, ninth Premier of British Columbia; and Robert Bonner, a powerful minister in the W.A.C. Bennett cabinet, and later CEO of MacMillan Bloedel and BC Hydro.
Nairn Falls Provincial Park is a provincial park in British Columbia, Canada located on the Green River adjacent to British Columbia Highway 99 and the Canadian National Railway line just south of Pemberton and less than twenty minutes north of the resort town of Whistler. The 170 hectare park was established in 1966, shortly after the highway's opening, to protect and enhance visitor access to Nairn Falls.
The British Columbia Interior, popularly referred to as the BC Interior or simply the Interior, is a geographic region of the Canadian province of British Columbia. While the exact boundaries are variously defined, the British Columbia Interior is generally defined to include the 14 regional districts that do not have coastline along the Pacific Ocean or Salish Sea, and are not part of the Lower Mainland. Other boundaries may exclude parts of or even entire regional districts, or expand the definition to include the regional districts of Fraser Valley, Squamish–Lillooet, and Kitimat–Stikine.
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,.
The Bridge River Country is a historic geographic region and mining district in the Interior of British Columbia, Canada, lying between the Fraser Canyon and the valley of the Lillooet River, south of the Chilcotin Plateau and north of the Lillooet Ranges. "The Bridge River" can mean the Bridge River Country as opposed to the Bridge River itself, and is considered to be part of the Lillooet Country, but has a distinct history and identity within the larger region. As Lillooet is sometimes considered to be the southwest limit of the Cariboo, some efforts were made to refer to the Bridge River as the "West Cariboo" but this never caught on.
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.
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.
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 New Westminster Land District is one of 59 land districts of British Columbia, Canada, which are the underlying cadastral divisions of that province, 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.
The Osoyoos Division Yale Land District is one of the 59 land districts of British Columbia, Canada, which are the underlying cadastral divisions of that province. 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.
The Cassiar 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.
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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.