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Taseko Lake
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 hy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taseko River
The Taseko River or Dasiqox in the original Chilcotin, is a tributary of British Columbia's Chilko River, a tributary of the Chilcotin River which joins the Fraser near the city of Williams Lake. The Taseko has its origins at Taylor Pass in the heart of an alpine area known as the South Chilcotin. Taylor Pass connects with Slim Creek, a major tributary of Gun Creek, which feeds the Bridge River via Carpenter Lake. From its source, it flows north then northwest before entering the south end of Upper Taseko Lake next to the Lord River, one of its major tributaries. The Tchaikazan River, another large tributary, also joins the river via the Taseko Lakes, entering at the area that separates Upper and Lower Taseko Lake. At the outlet of the two Taseko Lakes the river issues onto the broad Chilcotin Plateau. From source to Upper Taseko Lake, the Taseko is about 30 kilometres in length. From Lower Taseko Lake to the Taseko's confluence with the Chilko River is about 85 kilom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilcotin River
The Chilcotin River /tʃɪlˈkoʊtɪn/ located in Southern British Columbia, Canada is a long tributary of the Fraser River. The name Chilcotin comes from Tŝilhqot’in, meaning "ochre river people," where ochre refers to the mineral used by Tŝilhqot’in Nation and other Indigenous communities as a base for paint or dye. The Chilcotin River, Chilko River and Lake, and Taseko River and Lake make up the Chilcotin River watershed. This watershed drains the Chilcotin Plateau which reaches north to south from the Nechako Plateau to Bridge River county and east to west from Fraser River to the Coast Mountains. It is also one of twelve watersheds that make up the Fraser River Basin. Made up of seven major tributaries, Chilcotin River starts northeast of Itcha Mountain, flowing southeast until it joins the Fraser River south of Williams Lake, upstream from Gang Ranch. The geological processes that created this region support its diverse history, climate, and ecology. This d ... [...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 o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gunn Valley
Gunn Valley is a valley in the southern Chilcotin District of the Central Interior of British Columbia, Canada, just west of the Taseko Lakes and, like them, running on a north–south axis and at a perpendicular angle to Yohetta Valley, which drains to it via Yohetta Creek but also connects through a low pass to Chilko Lake farther west. In Gunn Valley are Tuzcha and Fishem Lakes, which are fed and drained by Yohetta Creek, which joins the Tchaikazan River at the valley's southern end. Lastman Lake is at the valley's north end and is connected to the other lakes by a swampy pass, through which runs the access road to Yohetta Valley. There is an airstrip near the valley's southern end. Name origin The valley's name is not derived from the Scots-Norwegian surname Gunn, but from the name of a member of the Xeni Gwet'in people of Nemaiah Valley Nemaiah Valley, also spelled Nemiah Valley and Nemaia Valley, is an unincorporated locality and First Nations reserve and ranching com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilcotin War
The Chilcotin War, the Chilcotin Uprising or the Bute Inlet Massacre was a confrontation in 1864 between members of the Tsilhqot'in (Chilcotin) people in British Columbia and white road construction workers. Fourteen men employed by Alfred Waddington in the building of a road from Bute Inlet were killed, as well as a number of men with a pack-train near Anahim Lake and a settler at Puntzi Lake. Background In 1862, Alfred Waddington began lobbying the press and his political allies for support to build a wagon road from Bute Inlet to Fort Alexandria, where it would connect to the Cariboo Road and continue on to the goldfields at Barkerville. He received approval for the construction early in 1863. According to Waddington, it would reduce land travel from to and the total days consumed in packing freight from 37 days to 22 compared to the route through Yale and the Fraser Canyon known as the Cariboo Road and favoured by Governor Douglas. The Bute Inlet Wagon Road was to follow t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brittany Triangle
Brittany (; french: link=no, Bretagne ; br, Breizh, or ; Gallo: ''Bertaèyn'' ) is a peninsula, historical country and cultural area in the west of modern France, covering the western part of what was known as Armorica during the period of Roman occupation. It became an independent kingdom and then a duchy before being united with the Kingdom of France in 1532 as a province governed as a separate nation under the crown. Brittany has also been referred to as Little Britain (as opposed to Great Britain, with which it shares an etymology). It is bordered by the English Channel to the north, Normandy to the northeast, eastern Pays de la Loire to the southeast, the Bay of Biscay to the south, and the Celtic Sea and the Atlantic Ocean to the west. Its land area is 34,023 km2 . Brittany is the site of some of the world's oldest standing architecture, home to the Barnenez, the Tumulus Saint-Michel and others, which date to the early 5th millennium BC. Today, the historical pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
