|
Tyoax Pass
Tyoax Pass is a mountain pass in the Chilcotin Ranges of the Pacific Ranges, the southernmost main subdivision of the Coast Mountains of British Columbia, Canada. Located at the head of Tyaughton Creek, a north tributary of the Bridge River, it connects the basin of the Bridge River with that of Big Creek in the southern Chilcotin District, and is therefore at the boundary between the Spruce Lake Protected Area and Big Creek Provincial Park. Name "Tyoax", pronounced "TIE-ax" in English, is a variant of "Tyaughton", which is from a Chilcotin language word meaning "jumping fish" and is also the name of Tyaughton Lake. See also *List of mountain passes This is a list of mountain passes. Africa Egypt * Halfaya Pass (near Libya) Lesotho * Moteng Pass * Mahlasela pass * Sani Pass Morocco * Tizi n'Tichka South Africa * Eastern Cape Passes * Western Cape Passes * Northern Cape Passes * Kwa ... References Mountain passes of British Columbia Chilcotin Ranges Landform ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ... [...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] |
Mountain Passes Of British Columbia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountain Passes
This is a list of mountain passes. Africa Egypt * Halfaya Pass (near Libya) Lesotho * Moteng Pass * Mahlasela pass * Sani Pass Morocco * Tizi n'Tichka South Africa * Eastern Cape Passes * Western Cape Passes * Northern Cape Passes * KwaZulu Natal Passes * Free State Passes * Limpopo Province Passes * Mpumalanga Passes * Gauteng Passes * Northwest Province Passes * Swartberg Pass (Western Cape) * Lootsberg Pass Asia Afghanistan * Broghol Pass to Pakistan * Dorah Pass to Pakistan * Hajigak Pass * Khost-Gardez Pass * Khyber Pass to Pakistan * Kotal-e Khushk * Kushan Pass linking northern Afghanistan to the region. * Lataband Pass * Tang-e Gharu is a gorge which links Afghanistan with Pakistan * Salang Pass crosses the Hindu Kush linking Kabul with northern Afghanistan - nowadays through a tunnel. * Wakhjir Pass to China China * Pingxingguan Pass, Shanxi * Jiayu Pass, Beijing * Jianmen Pass, Sichuan * Niangzi Pass, Border between Shanxi and Hebei * Yanmen Pass, Shan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyaughton Lake
Tyaughton Lake, also known as Tyax Lake, is a lake in the Bridge River Country of the West-Central Interior of British Columbia, Canada, located to the north of Carpenter Lake, a reservoir along the Bridge River formed by Terzaghi Dam of the Bridge River Power Project. Among the largest of a number of well-known fishing lakes located in valleys flanking the Bridge River, its name is an adaptation of a Chilcotin word meaning "jumping fish". Around its shores is a community of recreational homes, and near its southern end had been an older fishing lodge, the Tyaughton Lake Lodge, while on its northwestern shore is the Tyax Mountain Lake Resort, built in the 1980s, which at the time of construction was the largest log structure built in British Columbia in the 20th Century. Despite the shared name, it is not directly on the course of Tyaughton Creek, but is linked to the lower canyon of that creek by a short intermediary stream. The main road access is from the Gun Creek Forest Se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilcotin Language
''Nenqayni Ch’ih'' (lit. "the Native way") (also Chilcotin, Tŝilhqotʹin, Tsilhqot’in, Tsilhqút’in) is a Northern Athabaskan language spoken in British Columbia by the Tsilhqot’in people. The name ''Chilcotin'' is derived from the Chilcotin name for themselves: , literally "people of the red ochre river". Phonology Consonants Chilcotin has 47 consonants: * Like many other Athabaskan languages, Chilcotin does not have a contrast between fricatives and approximants. * The alveolar series is pharyngealized. * Dentals and alveolars: ** Both Krauss (1975) and Cook (1993) describe the dental and alveolar as being essentially identical in articulation, ''postdental'', with the only differentiating factor being their different behaviours in the vowel flattening processes (described below). **Gafos (1999, personal communication with Cook) describes the dental series as ''apico-laminal denti-alveolar'' and the alveolar series as ''lamino-postalveolar''. Vowels Chilcotin has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Creek Provincial Park
Big Creek Provincial Park is a provincial park in British Columbia, Canada. It is adjoined on the south by the Spruce Lake Protected Area (a.k.a. the South Chilcotin or Southern Chilcotins, though in the Bridge River Country) and on the west by Tsʼilʔos Provincial Park. Neighbouring on the east is the Churn Creek Protected Area The Churn Creek Protected Area is a provincial protected area in British Columbia, Canada. It is a mix of dryland canyon and steppe and adjoining rangeland flanking the canyon of Churn Creek and that stream's confluence with the Fraser River at .... The park was first established in 1995 and expanded in 2000, 2001 and 2004 to total approximately 67,918 hectares. References Provincial parks of British Columbia Geography of the Chilcotin Chilcotin Ranges 1995 establishments in British Columbia Protected areas established in 1995 {{BritishColumbia-park-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spruce Lake Protected Area
The Spruce Lake Protected Area, formerly known variously as the Southern Chilcotin Mountains Provincial Park, Southern Chilcotins, and also as South Chilcotin Provincial Park, is a 71,347-hectare Protected Area in the British Columbia provincial parks system, approximately 200 km north of Vancouver. The area had been the subject of an ongoing preservationist controversy since the 1930s. In 2007, its status as a provincial park was downgraded to protected area. Recreational activities in the park included hiking, cycling, swimming, fishing and hunting, and there were walk-in wilderness camping sites. Wildlife in the protected area include grizzly bear, California bighorn sheep and wolverine. In June 2010, Bill 15 created the South Chilcotin Mountains Park, a "Class A" park of 56,796 hectares, from Spruce Lake Protected Area. The remaining approximately 14,550 hectares were set aside for tourism and mining, but commercial logging is still prohibited. The bill also confirmed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Creek (British Columbia)
Big Creek is a roughly long tributary of British Columbia's Chilcotin River. Its source is remote Lorna Lake, located deep in the midst of the Chilcotin Ranges, near the vertex of the boundaries of Big Creek Provincial Park, the valley of the Taseko River and Taseko Lakes, which lies to its west, and the Spruce Lake Protected Area to its south (aka the "South Chilcotin" even though it is in the Bridge River Country, part of the Lillooet region). Near Lorna Lake is a location known as Graveyard Valley, believed to be the site of the final battle of a 19th-century war between the Tsilhqot'in and St'at'imc peoples over control of the upper basin of the Bridge River, which lies over the mountains to the south of Big Creek. The Big Creek basin is the easternmost of three southern tributary basins of the Chilcotin, the others to its west being the Taseko River basin and, west of it, the Chilko River basin. The largest stream to its east is Churn Creek, whose headwater creeks sh ... [...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] |
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 Fraser's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyaughton Creek
Tyaughton Creek, formerly gazetted as the Tyaughton River, also historically known as Tyoax Creek, is a 50 kilometre tributary of British Columbia's Bridge River, flowing generally southeast to enter the main flow of that river about mid-way along the length of Carpenter Lake, a reservoir formed by Terzaghi Dam of the Bridge River Power Project. Course The creek begins at Tyoax Pass, at the divide between the basins of the Bridge River and that of Big Creek, which is a tributary of the Chilcotin River. Its upper course flows east, then turns south and then southeast, entering a progressively deeper canyon until just northeast of Tyaughton Lake, which is connected to it by a short creek, and then turns east-southeast between Pearson Ridge (SW) and Marshall Ridge (NE) in a continuation of its canyon until it emerges as a side-inlet of Carpenter Lake which was formed by the creation of Carpenter Lake. That inlet is bridged at the mouth of that inlet by BC Highway 40, also known as t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
