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Shulaps
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 e ... [...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 Sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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] |
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 extensive ... [...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 sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Minto City, British Columbia
Minto City, often called just Minto, sometimes Minto Mines, Minto Mine, Skumakum, or "land of plenty", was a gold mining town in the Bridge River Valley of British Columbia from 1930 to 1936, located at the confluence of that river with Gun Creek, one of its larger tributaries. The mine prospect was never much successful although a model townsite was built by promoter "Big Bill" Davidson, who imported soil to build a specially-built rodeo ground and baseball diamond on the rocky site. The larger mine of Bralorne was nearby. The mine shut down in 1936 due to productivity issues, but restarted in 1940. The valley has since been significantly altered when most of the vestiges of the town were inundated by the waters of the Carpenter Lake reservoir following completion of the Bridge River Power Project. In 1941, around two dozens of Japanese Canadian families were relocated to Minto Mine, and ordered to live in the empty miners' houses due to the impacts of the war. The community w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
St'at'imcets Language
Lillooet , known in the language itself as / (), is the language of the St’át’imc, a Salishan language of the Interior branch spoken in southern British Columbia, Canada, around the middle Fraser and Lillooet Rivers. The language of the Lower Lillooet people uses the name ', because ' means "the language of the people of ''Sat̓''", i.e. the Upper Lillooet of the Fraser River. Lillooet is an endangered language with as few as 200 native speakers practically all of whom are over 60 years of age (Gordon 2005). Regional varieties St̓át̓imcets has two main dialects: * ''Upper/Northern St̓át̓imcets'' ( St̓át̓imcets, Fountain) * ''Lower/Southern St̓at̓imcets'' (a.k.a. Lil̓wat7úlmec, Mount Currie) Upper St̓át̓imcets is spoken around Fountain, Pavilion, Lillooet, and neighboring areas. Lower St̓át̓imcets is spoken around Mount Currie and neighboring areas. An additional subdialect called Skookumchuck is spoken within the Lower St̓át̓imcets dialec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gold Bridge, British Columbia
Gold Bridge is an unincorporated community in the Bridge River Country of British Columbia, Canada. Although numbering only around 40 inhabitants, Gold Bridge is the service and supply centre for the upper basin of the Bridge River Valley, which includes recreation-residential areas at the Gun Lakes, Tyaughton Lake, Marshall Creek, and Bralorne; and the nearby ghost towns of Brexton and Pioneer Mine. Located at the confluence of the Bridge River with its south fork, the Hurley River, Gold Bridge began as a freewheeling merchandising and services center supplementary to the company-run gold mining towns, and in its heyday had a large commercial roster ranging from insurance and stockbrokers through to bootleggers and " sporting houses". Gold Bridge can be accessed via Highway 40 from Lillooet, or via an upgraded backroad from Pemberton and Whistler known as the Hurley Main, which uses a pass at the head of the Hurley River to access the valley of the upper Lillooet River no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bralorne, British Columbia
Bralorne ( ) is a historic Canadian gold mining community in the Bridge River District of British Columbia, some 130 km on dirt roads west of the town of Lillooet. Background Gold has been the central element in the area's history going back to the 1858-1860 Fraser River Gold Rush. Miners rushed to the Cayoosh and Bridge River areas looking for placer deposits, One named Cadwallader looked for the outcroppings on the creek that is now named for him and turned out later to be the site of the richest hard-rock veins in the region. Early exploratory parties of Chinese and Italians in the upper Bridge River basin were driven out by Chief Hunter Jack, who himself had a secret placer mine somewhere in the region, believed to be in upper Tyaughton Creek. and whose big-game hunting territory this also was. During the 1870s Hunter Jack began to invite chosen prospectors into the valley, and ran a ferry across the Bridge River that virtually all entering the region had to cross. Am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpenter Lake Reservoir
Carpenter Lake, officially Carpenter Lake Reservoir, is the largest of the three reservoirs of the Bridge River Power Project, which is located in the mountains west of Lillooet, British Columbia. The lake is about 185 kilometres north of the province's major city of Vancouver and is formed by the 1951 diversion of the Bridge River by Terzaghi Dam into Seton Lake via a tunnel through Mission Mountain, which separates the Seton and Bridge drainages. Several ranches and homesteads in the broad serpentine of the upper Bridge River basin were flooded out by the hydro project, which changed the character of the upper valley forever. Carpenter Lake is about 50 kilometres in length, although its upper reaches beyond the flooded gold mining town of Minto City are usually mudflat due to fluctuations in the level of the reservoir. Its total area approaches 50 square kilometres. Name The lake is named after a Mr. Carpenter, an engineer who first moved to Canada in 1909 and performed much ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
