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Taseko Mountain
Taseko Mountain, also known as Mount Taseko (pronounced ''Ta-SEE-ko'') 3063 m (10049 ft), prominence: 1277 m, is one of the principal summits of the Chilcotin Ranges, part of the Pacific Ranges subdivision of the Coast Mountains of southern British Columbia. Standing just east of the Taseko Lakes, it is the highest summit between the Taseko Lakes and the Fraser River, and the highest east of the pass between the basins of the Lord and Bridge Rivers. North and east of Taseko Mountain the landscape drops off dramatically to the flat Chilcotin Plateau. Immediately west across Taseko Lake is Mount Tatlow Tŝ’ilʔoŝ, also known as Mount Tatlow, is one of the principal summits of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains of southern British Columbia. Standing on an isolated ridge between the lower end of ..., which has the same elevation as Taseko Mountain. References Three-thousanders of British Columbia Landforms of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilcotin Ranges
The Chilcotin Ranges are a subdivision of the Pacific Ranges of the Coast Mountains (in some classifications they are a separate subdivision). They lie on the inland lea of the Pacific Ranges, abutting the Interior Plateau of British Columbia. Their northwestern end is near the head of the Klinaklini River and their southeast end is the Fraser River just north of Lillooet; their northern flank is the edge of the Plateau while their southern is the north bank of the Bridge River. In some reckonings they do not go all the way to the Fraser but end at the Yalakom River, which is the North Fork of the Bridge. They are not one range but a collection of ranges, often very distinct from each other. There are three major named subranges: * Dickson Range * Shulaps Range *Camelsfoot Range (assigned to the Interior Plateau in some definitions) To the west of the western end of the Chilcotin Ranges, and considered by some to be part of the group, are: *Pantheon Range * Niut Range South ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taseko Lakes
The Taseko Lakes are a pair of lakes, Upper Taseko Lake and Lower Taseko Lake, which are expansions of the upper Taseko River in the southern Chilcotin District of the Central Interior of British Columbia, Canada. Their name is based on the original in the Chilcotin language, Dasiqox Biny, where "Desiqox" means "Mosquito River" and is cognate to the name of the river as in English; the Chilcotin name refers to both lakes as one lake, which was also originally the case with the English usage until official designation of the separate lakes in 1954. The lakes are separated by the short Taseko Narrows, the name of which in Chilcotin is ''nanats'akash'', and is an important crossing place for deer. The Tchaikazan River flows the area between the upper & lower lake from the southwest, while the Taseko River feeds it from the southeast, while the equally large Lord River joins it from the south, at the head of the lake. History The Taseko Lakes were proposed to be part of a massive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of British Columbia
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tatlow
Tŝ’ilʔoŝ, also known as Mount Tatlow, is one of the principal summits of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains of southern British Columbia. Standing on an isolated ridge between the lower end of Chilko Lake and the Taseko Lakes, it is in elevation. Southeast across the Taseko Lakes is Taseko Mountain , the highest summit between those lakes and the Fraser River, while directly south beyond Yohetta Valley (a deep valley which connects the relative lowlands around Chilko and Taseko Lakes is the massif containing Monmouth Mountain . Southwest across Chilko Lake is Mount Good Hope and due west, also across Chilko Lake, is Mount Queen Bess , the highest peak east of the Homathko River before the Waddington Range massif, which is at the core of the range and contains Mount Waddington . Name The name Mount Tatlow was officially adopted on 26 June 1911, as submitted on 23 June 1910 by Sidney Williams, and on 11 March 2019, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilcotin District
The Chilcotin () region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River. Chilcotin is also the name of the river draining that region. In the language of the Chilcotin people their name and the name of the river means "people of the red ochre river" (its tributary the Chilko River means "red ochre river") The Chilcotin district is often viewed as an extension of the Cariboo region, east of that river, although it has a distinct identity from the Cariboo District. It is, nonetheless, part of the Cariboo Regional District which is a municipal-level body governing some aspects of infrastructure and land-used planning. The vast majority of the population are First Nations people, members of the Tsilhqot'in and Dakelh peoples, while others are settlers and ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bridge River
The Bridge River is an approximately long river in southern British Columbia. It flows south-east from the Coast Mountains. Until 1961, it was a major tributary of the Fraser River, entering that stream about six miles upstream from the town of Lillooet; its flow, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project, with the water now entering the Fraser just south of Lillooet as a result. The Bridge River hydroelectric complex, operated by BC Hydro, consists of three successive dams, providing water for four hydro power plants with the total rated power of total 492 megawatts. Name Its name in the Lillooet language is Xwisten (pronounced Hwist'n), sometimes spelled Nxwisten or Nxo-isten). Dubbed ''Riviere du Font'' by Simon Fraser's exploring party in 1808, it was for a while known by the English version of that name, ''Fountain River'', and some old maps show it as Shaw's River, after the name of one of Frase ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lord River (Canada)
The Lord River is a tributary of the Taseko River in the southern Chilcotin District of the Central Interior of British Columbia, Canada, joining that river via the head of Upper Taseko Lake, which is also fed by the upper reaches of the Taseko River proper. The Lord River rises in the area of Lord Pass, which connects to the headwater area of the Bridge River The Bridge River is an approximately long river in southern British Columbia. It flows south-east from the Coast Mountains. Until 1961, it was a major tributary of the Fraser River, entering that stream about six miles upstream from the town of ... immediately south. See also * Tchaikazan River * Tsy'los Provincial Park References * Rivers of the Pacific Ranges Rivers of the Chilcotin Chilcotin Ranges Lillooet Land District {{BritishColumbiaInterior-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fraser River
The Fraser River is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for , into the Strait of Georgia just south of the City of Vancouver. The river's annual discharge at its mouth is or , and it discharges 20 million tons of sediment into the ocean. Naming The river is named after Simon Fraser, who led an expedition in 1808 on behalf of the North West Company from the site of present-day Prince George almost to the mouth of the river. The river's name in the Halqemeylem (Upriver Halkomelem) language is , often seen archaically as Staulo, and has been adopted by the Halkomelem-speaking peoples of the Lower Mainland as their collective name, . The river's name in the Dakelh language is . The ''Tsilhqot'in'' name for the river, not dissimilar to the ''Dakelh'' name, is , meaning Sturgeon ''()'' River ''()''. Course The Fraser drains a area. Its source is a dripping spring at Fras ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coast Mountains
The Coast Mountains (french: La chaîne Côtière) are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the Coast of British Columbia south to the Fraser River. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. The Coast Mountains are part of a larger mountain system called the Pacific Coast Ranges or the Pacific Mountain System, which includes the Cascade Range, the Insular Mountains, the Olympic Mountains, the Oregon Coast Range, the California Coast Ranges, the Saint Elias Mountains and the Chugach Mountains. The Coast Mountains are also part of the American Cordilleraa Spanish term for an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pacific Ranges
, photo = Mount Garibaldi (50997016501).jpg , photo_size = 280px , photo_caption = Mount Garibaldi massif as seen from Squamish , map = , map_image = South BC-NW USA-relief PacificRanges.png , map_caption = Pacific Ranges as defined in S. Holland ''Landforms of British Columbia'' , map_relief = , map_size = 280px , highest = Mount Waddington , area_km2 = 108237 , elevation_m = 4019 , elevation_ref = , prominence_m = , prominence_ref = , isolation_km = , isolation_ref = , coordinates = , coordinates_ref = , location = British Columbia, Canada , parent = Coast Mountains , type = , age = , geology = , volcanic_arc = , volcanic_belt = , volcanic_field = , volcanic_arc/belt = , last_eruption = , embedded = The Pacific Ranges are the southe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mapp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lillooet Land District
The Lillooet Land District is one of the 59 Cadastre, cadastral subdivisions of British Columbia, which were created by the Lands Act of the Colony of British Columbia (1858-1866), 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 (electoral district), 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 Country, 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, British ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
