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Camelsfoot Range
The Camelsfoot Range is a sub-range of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains in British Columbia. The Fraser River forms its eastern boundary. The range is approximately 90 km at its maximum length and less than 30 km wide at its widest. Terrain and location The far southeast end of the Camelsfoot is extremely rugged, and dropping to one last point at 7000'-plus before plunging into the gorge of the Fraser Canyon at Fountain, near Lillooet. For 45 km NW from there, the range is rocky and lightly forested with lodgepole pine, breaking into high benchlands and large creek basins draining through benchland country via small canyons. Beyond that the range's terrain is much more gentle, with high, meadowed ridges running east towards the Fraser Canyon between treed plateaus and small canyons, and a few large, barren domes running further north along the Fraser. The range is bounded on the north and west by a large and impressive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Provinces And Territories Of Canada
Within the geographical areas of Canada, the ten provinces and three territories are sub-national administrative divisions under the jurisdiction of the Canadian Constitution. In the 1867 Canadian Confederation, three provinces of British North America—New Brunswick, Nova Scotia, and the Province of Canada (which upon Confederation was divided into Ontario and Quebec)—united to form a federation, becoming a fully independent country over the next century. Over its history, Canada's international borders have changed several times as it has added territories and provinces, making it the world's second-largest country by area. The major difference between a Canadian province and a territory is that provinces receive their power and authority from the ''Constitution Act, 1867'' (formerly called the ''British North America Act, 1867''), whereas territorial governments are creatures of statute with powers delegated to them by the Parliament of Canada. The powers flowing from t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Douglas Road
The Douglas Road, a.k.a. the Lillooet Trail, Harrison Trail or Lakes Route, was a goldrush-era transportation route from the British Columbia Coast to the Interior (NB another route known as the Lillooet Trail was the Lillooet Cattle Trail, which used some of the same route but was built 25 years later). Over 30,000 men are reckoned to have travelled the route in, although by the end of the 1860s it was virtually abandoned due to the construction of the Cariboo Wagon Road, which bypassed the region. History Originally traversed by Hudson's Bay Company employees in 1828 and charted by HBC explorer Alexander Caulfield Anderson in 1846, the route was heavily travelled by prospectors seeking to avoid the dangers of the Fraser Canyon to access the gold-bearing bars of the Fraser around today's Lillooet. Pressure for an alternative route to the Upper Fraser had mounted in the wake of the Fraser Canyon War of the winter of 1859, and miners were wary of travelling through the territory ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Nations In Canada
First Nations (french: Premières Nations) is a term used to identify those Indigenous Canadian peoples who are neither Inuit nor Métis. Traditionally, First Nations in Canada were peoples who lived south of the tree line, and mainly south of the Arctic Circle. There are 634 recognized First Nations governments or bands across Canada. Roughly half are located in the provinces of Ontario and British Columbia. Under Charter jurisprudence, First Nations are a "designated group," along with women, visible minorities, and people with physical or mental disabilities. First Nations are not defined as a visible minority by the criteria of Statistics Canada. North American indigenous peoples have cultures spanning thousands of years. Some of their oral traditions accurately describe historical events, such as the Cascadia earthquake of 1700 and the 18th-century Tseax Cone eruption. Written records began with the arrival of European explorers and colonists during the Age of Dis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hat Creek (British Columbia)
Hat Creek is a tributary of the Bonaparte River in British Columbia, Canada, joining that stream at Carquile, British Columbia, Carquile, which is also known as Lower Hat Creek, British Columbia, Lower Hat Creek and is the site of the Hat Creek Ranch heritage museum and visitor centre. The Hat Creek basin includes a broad upper plateau area encircled by the gentle but high summits of the Clear Range and, to its east, the Cornwall Hills; this area is known as Upper Hat Creek, British Columbia, Upper Hat Creek. Adjacent to Upper Hat Creek is the gateway to Marble Canyon (Canada), Marble Canyon and a rancherie of the Pavilion First Nation, who are both a St'at'imc and Secwepemc people. During the Fraser Canyon Gold Rush, Fraser Canyon and Cariboo Gold Rushes an important trail northwards from the lower Fraser Canyon led from Foster Bar on the Fraser via Laluwissen Creek into Upper Hat Creek, then via the creek to the Bonaparte River. The economy of the basin is ranching-based and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shulaps Range
The Shulaps Range is a subrange of the Chilcotin Ranges subset of the Pacific Ranges of the Coast Mountains in southwest-central British Columbia. The range is 55 km NW–SE and 15 km SW–NE and 2,970 km2 (1150 mi2) in area. The range is fairly high in elevation, with dryland-type summits with some very small icefields. Its highest summits are Shulaps Peak 2880 m (9449 ft) and Big Dog Mountain 2,862 m (9,390 ft). Another prominent summit is Rex Peak 2684 m (8806 ft), a conical mass dominating the southern end of the range, which is delimited by the buttress-wall of the Bridge River Canyon. Terrain and location The Shulaps' northeast flank is a series of high basins. Many contain alpine lakes and which allow for road access to high up in various parts of the range. There is an active gold claim on the south flank of Big Dog Mountain in the basin of Blue Creek in the northwestern part of the range and, at the far southeast en ... [...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] |
Yalakom River
The Yalakom River is a tributary of the Bridge River, which is one of the principal tributaries of the Fraser River, entering it near the town of Lillooet, British Columbia. In frontier times it was also known as the North Fork of the Bridge River, and joins the Bridge River proper at Moha, a rural community with a history in ranching, farming and mining. The river is approximately 50km (30 mi) in length. The valley's climate is semi-arid in character and lodgepole pine predominates below treeline. The name Yalakom comes from the Statimc language word for the ewe of the mountain sheep and is also applied to one of the major peaks of the Camelsfoot Range, which rises along the east bank of the Yalakom. West of the river is the Shulaps Range, which is similarly named for the ram of the mountain sheep in Statimc. The upper part of the valley's east bank, in the area of Yalakom Mountain, had been for many years a wildlife preserve and the area remains rich in game. The rural ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cariboo Alligator
The Cariboo is an intermontane region of British Columbia, Canada, centered on a plateau stretching from Fraser Canyon to the Cariboo Mountains. The name is a reference to the caribou that were once abundant in the region. The Cariboo was the first region of the interior north of the lower Fraser River and its canyon to be settled by non-indigenous people, and played an important part in the early history of the colony and province. The boundaries of the Cariboo proper in its historical sense are debatable, but its original meaning was the region north of the forks of the Quesnel River and the low mountainous basins between the mouth of that river on the Fraser at the city of Quesnel and the northward end of the Cariboo Mountains, an area that is mostly in the Quesnel Highland and focused on several now-famous gold-bearing creeks near the head of the Willow River. The richest of them all, Williams Creek, is the location of Barkerville, which was the capital of the Cariboo Gol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sasquatch
Bigfoot, also commonly referred to as Sasquatch, is a purported ape-like creature said to inhabit the forest of North America. Many dubious articles have been offered in attempts to prove the existence of Bigfoot, including Anecdotal evidence, anecdotal claims of sightings as well as alleged video and audio recordings, photographs, and casts of large footprints. Some are known or admitted hoaxes. Tales of wild, hairy humanoids exist throughout the world, and such creatures appear in the folklore of North America, including the Mythologies of the indigenous peoples of the Americas, mythologies of indigenous people. Bigfoot is an icon within the fringe subculture of cryptozoology, and an enduring element of popular culture. The majority of mainstream scientists have historically discounted the existence of Bigfoot, considering it to be the result of a combination of folklore, misidentification, and hoax, rather than a living animal. Folkloristics, Folklorists trace the phenomenon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Interior Plateau
The Interior Plateau comprises a large region of the Interior of British Columbia, and lies between the Cariboo and Monashee Mountains on the east, and the Hazelton Mountains, Coast Mountains and Cascade Range on the west.''Landforms of British Columbia'', S. Holland, Government of British Columbia'' The continuation of the plateau into the United States is known there as the Columbia Plateau. Physiographically, the Interior Plateau is a section of the larger Northern Plateaus province, which in turn is part of the Intermontane Plateaus physiographic division. (The Interior Plateau is ''not'' part of the Interior Mountains, a huge area that constitutes most of the northern two thirds of the Canadian province of British Columbia between the Coast Mountains, Rocky Mountains and the various small ranges on the inland lea of the Coast Mountains between the Bulkley Ranges and the Bella Coola River). Subdivisions It has several subdivisions, these being: * The Fraser Plateau ** The Chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashcroft, British Columbia
Ashcroft ( 2016 population: 1,558) is a village in the Thompson Country of the Interior of British Columbia, Canada. It is downstream from the west end of Kamloops Lake, at the confluence of the Bonaparte and Thompson Rivers, and is in the Thompson-Nicola Regional District. Ashcroft's downtown is on the east side of the Thompson River, although the municipal boundaries straddle the river, with housing and the town's hospital and recreation complex on the west bank. It is something of a "twin" to nearby Cache Creek, which unlike Ashcroft is on the major highway. History Ashcroft was named after the nearby Ashcroft Manor on Ashcroft Ranch founded in the 1860s, during the Cariboo Gold Rush, by two English brothers named Clement Francis Cornwall and Henry Pennant Cornwall, who emigrated to Canada from Ashcroft, at Newington Bagpath in Gloucestershire. The brothers had originally come in search of gold; however, on hearing stories from failed gold searchers they decided to found t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yale, British Columbia
Yale is an unincorporated town in the Canadian province of British Columbia, which grew in importance during the gold rush era. Located on the Fraser River, it is generally considered to be on the dividing line between the Coast and the Interior regions of the British Columbia Mainland. Immediately north of the town, the Fraser Canyon begins and the river is generally considered unnavigable past this point. Rough water is common on the Fraser anywhere upstream from Chilliwack and even more so above Hope, about south of Yale. However, steamers could make it to Yale, good pilots and water conditions permitting, and the town had a busy dockside life as well as a variety of bars, restaurants, hotels, saloons and various services. Its maximum population during the gold rush era was in the 15,000 range. More generally, it housed 5,000-8,000. The higher figure was counted at the time of evacuation of the Canyon during the Fraser Canyon War of 1858. Most of today's population are membe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_at_Yale%2C_BC_on_Fraser_River_1882.JPG "Click for more on -> Yale, British Columbia")