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Skihist Mountain
Skihist Mountain, also sometimes referred to as Skihist Peak, is the highest mountain in the Cantilever Range and in southwestern British Columbia, Canada. It is located on the southern boundary of Stein Valley Nlaka'pamux Heritage Park, about west of Lytton. It is the highest summit in the Lillooet Ranges, which lie between the Lillooet and Fraser Rivers, south of the Gates Valley and Seton and Anderson Lakes. Skihist Mountain consists of a north–south aligned ridge. Kent Creek drains its northern slopes while Nesbitt Creek drains the south and west slopes. Both creeks feed the Stein River. On its eastern slopes, it is drained by North Kwoiek Creek, which originates at Skihist Lake, a small mountain lake located approximately three kilometres southeast of Skihist's summit. The peak is most easily climbed via its south slopes, from the North Kwoiek Creek drainage. Name origin According to ethnologist James Teit, writing in 1917, the word ''skihist'' means "jump" or "lea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cantilever Range
The Cantilever Range is a mountain range in southwestern British Columbia, Canada, a subrange of the Lillooet Ranges, which is itself a subgrouping of the Pacific Ranges of the Coast Mountains. About 1100 km2 in area and about 50 km east to west and 35 km north to south, the Cantilever Range is located southwest of Lytton between the valleys of the Stein River (N) and Kwoiek Creek (S). The Cantilever Range is the highest sector of the Lillooet Ranges and is crowned by Skihist Mountain, which stands in elevation, making it the highest mountain in southwestern British Columbia. The next-highest is nearby Petlushkwohap Mountain Petlushkwohap Mountain is a mountain in the Cantilever Range, located west of the town of Lytton, British Columbia, Canada, in that province's Fraser Canyon region. The Cantilever Range is a small subrange of the Lillooet Ranges, the southeaster ..., standing . Most other peaks in the range, which is really a ridge between the two watershe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lillooet River
The Lillooet River is a major river of the southern Coast Mountains of British Columbia. It begins at Silt Lake, on the southern edge of the Lillooet Crown Icecap about 80 kilometres northwest of Pemberton and about 85 kilometres northwest of Whistler. Its upper valley is about 95 kilometres in length, entering Lillooet Lake about 15 km downstream from Pemberton on the eastern outskirts of the Mount Currie reserve of the Lil'wat branch of the St'at'imc people. From Pemberton Meadows, about 40 km upstream from Pemberton, to Lillooet Lake, the flat bottomlands of the river form the Pemberton Valley farming region. Below the 30 km (18.6 mi) length of Lillooet Lake, it resumes again just north of the native community and ghost town of Skookumchuck Hot Springs, which is known in the St'at'imcets language as Skatin. The lower stretch of the Lillooet River, from Lillooet Lake to Harrison Lake, is approximately 55 km (c. 34 mi) in length. Its main ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of British Columbia
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petlushkwohap Mountain
Petlushkwohap Mountain is a mountain in the Cantilever Range, located west of the town of Lytton, British Columbia, Canada, in that province's Fraser Canyon region. The Cantilever Range is a small subrange of the Lillooet Ranges, the southeasternmost subrange of the Pacific Ranges of the Coast Mountains. Petlushkwohap is the second-highest summit in the Lillooet Ranges, after nearby Skihist Mountain Skihist Mountain, also sometimes referred to as Skihist Peak, is the highest mountain in the Cantilever Range and in southwestern British Columbia, Canada. It is located on the southern boundary of Stein Valley Nlaka'pamux Heritage Park, about ... and is one of the mountains within the Stein Valley Nlaka'pamux Heritage Park. References {{reflist Two-thousanders of British Columbia Lillooet Ranges Fraser Canyon Yale Division Yale Land District ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of British Columbia
British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. Statist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skihist Provincial Park
Skihist Provincial Park is a provincial park in British Columbia, Canada, located on the Thompson River and adjacent to the Trans-Canada Highway #1 between the towns of Lytton (W) and Spences Bridge (E). The park is named for Skihist Mountain, which is visible from the park though on the opposite side of the Fraser River to the west of Lytton. History Skihist Provincial Park was established in 1956 as a rest stop and overnight camping location along highway 1 The following highways are numbered 1. For roads numbered A1, see list of A1 roads. For roads numbered B1, see list of B1 roads. For roads numbered M1, see List of M1 roads. For roads numbered N1, see list of N1 roads. For roads numbered .... Facilities Day-Use Adjacent to the highway, a rest area with water and flush toilets is available. There are standard parking spots as well as trailer parking spots. The rest area closes for the winter season. The park is open from May to September. Camping Skihist Campgro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akasik Mountain
Akasik Mountain is a mountain in the Lillooet Ranges of British Columbia, Canada, located southwest of the town of Lytton. The mountain is associated in the lore of the Nlaka'pamux people with Skihist Mountain Skihist Mountain, also sometimes referred to as Skihist Peak, is the highest mountain in the Cantilever Range and in southwestern British Columbia, Canada. It is located on the southern boundary of Stein Valley Nlaka'pamux Heritage Park, about ..., whose name means "jump" or "leap" and is a reference to a mythological giant who leapt back and forth between Skihist and this summit. References {{Pacific Ranges Fraser Canyon Lillooet Ranges Two-thousanders of British Columbia Kamloops Division Yale Land District ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Teit
James Alexander Teit (15 April 1864 — 30 October 1922) was an anthropologist, photographer and guide who worked with Franz Boas to study Interior Salish First Nations peoples in the late 19th and early 20th centuries. He led expeditions throughout British Columbia and made many contributions towards native ethnology. He also worked with Edward Sapir of the Geological Survey of Canada in 1911. In the later part of his life Teit worked tirelessly with the native people to preserve their human rights, as discussed by Wendy Wickwire in her work ''At the Bridge''. Teit was born in Lerwick, Shetland, Scotland but immigrated to Canada and married a Nlaka'pamux woman named Susanna Lucy Antko. It was through his wife that he became knowledgeable of the culture and language Language is a structured system of communication. The structure of a language is its grammar and the free components are its vocabulary. Languages are the primary means by which humans communicate, and may be c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stein River
The Stein River is a tributary of the Fraser River in the Canadian province of British Columbia. The name is derived from the Nlaka'pamux word Stagyn, meaning "hidden place", referring to the fact that the size and extent of the Stein River valley is not very noticeable from the river's confluence with the Fraser. It is one of only 2 unlogged watersheds with an area greater than 50 km south of Prince George, BC Prince George is the largest city in northern British Columbia, Canada, with a population of 74,004 in the metropolitan area. It is often called the province's "northern capital" or sometimes the "spruce capital" because it is the hub city for .... Course The Stein River and its tributaries are contained in Stein Valley Nlaka'pamux Heritage Park. The river originates in remote Tundra Lake and flows generally east, joining the Fraser River north of Lytton. See also * List of British Columbia rivers References Tributaries of the Fraser River Fraser Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anderson Lake (British Columbia)
Anderson Lake is located about 25 miles North of the town of Pemberton, British Columbia and is about 28.5 km2 (11 sq mi) in area and around 21 km (13 mi) in length. Its maximum depth is 215 meters (705 feet). It is drained by the Seton River, which feeds Seton Lake and so the Fraser River. It is fed by the Gates River, which drains from the Pemberton Pass divide with the Birkenhead River valley towards Pemberton- Mount Currie. It and Seton Lake were originally the same lake, which was cut in half between ten and twenty thousand years ago by a large landslide from the north face of the Cayoosh Range, which fronts Anderson Lake on the east. The slide created a locality known today as Seton Portage, which combined with the steamer ''Lady of The Lake'' played a key role on the route of the Douglas Road during the Fraser Canyon Gold Rush of 1858–59.http://www.library.ubc.ca/archives/pdfs/bchf/bchq_1946_1.pdf At its head, near the mouth of the Gates River, is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seton Lake
Seton Lake is a freshwater fjord draining east via the Seton River into the Fraser River at the town of Lillooet, about long, in area and lies at an elevation of . Its depth is . The lake is natural in origin but was raised slightly as part of the Bridge River Power Project, the two main powerhouses of which are on the north shore of the upper end of the lake near Shalalth. At the uppermost end of the lake is the community of Seton Portage and the mouth of the short Seton Portage River, which connects Anderson Lake on the farther side of the Portage to Seton Lake. The Seton Portage River is the main source of natural inflow to Seton Lake, and is primarily fed by Anderson Lake but also by Whitecap Creek, which has its origin on the east slopes of Whitecap Mountain, the highest in the Bendor Range, and by Spider Creek, which has its origin on the north slopes of an unnamed summit to the south of Seton Lake, which happens to be the highest of the Cayoosh Range which lines the sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gates Valley
The Gates Valley is a valley and group of communities in the Lillooet Country of the Southern Interior of British Columbia, Canada, located between the summit of Pemberton Pass and the head of Anderson Lake at the community of D'Arcy. Though the term strictly refers to the valley of the Gates River, it is usually used more in a sense of the communities located in the valley and is not a term used for the river's drainage basin, which is much larger. The valley was part of the route of the Douglas Road, which was built during the Fraser Canyon Gold Rush of 1858–1860. Birkenhead Lake Provincial Park is accessed from the Gates Valley, via a turnoff up Blackwater Creek near the community of Gates. The communities of the valley include: * Birken *Gates * Devine * D'Arcy/N'quatqua N'Quatqua, variously spelled Nequatque, N'quat'qua, is the proper historic name in the St'at'imcets language for the First Nations village of the Stl'atl'imx people of the community of D'Arcy, British Col ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
