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Bendor Range
The Bendor Range is a small but once-famous subrange of the Pacific Ranges of the Coast Mountains, about It is approximately 7,000 square kilometres (2,700 mi2) in area and about 40 km long (NW to SE) and about 18 km at its widest. It lies between Anderson Lake on the southeast and the Carpenter Lake Reservoir or the Bridge River Power Project on the north, with the gold-rich valley of Cadwallader Creek on its southwest. The range's western flank is the site of a series of now-semi-abandoned mining towns. One of these, Bralorne, is among the deepest mines in Canada and in its heyday was the third-richest gold mine in the world; it has waned from a peak population of 8,000 to less than 300 today. Its shafts plunge a mile beneath sea level under the range, starting at 3500' above. The name "Bendor" is believed by some locally to be a Gaelic-French hybrid - ''ben d'or'' - ''mountain of gold'' (note Welsh: Pen d'awr means the same thing) - and while it does mean th ...
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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 The Bridge River Power Project is a hydroelectric power development in the Canadian province of British Columbia, located in the Lillooet Country between Whistler and Lillooet. It harnesses the power of the Bridge River, a tributary of the .... 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 ...
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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 ...
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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 ...
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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 ...
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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 th ...
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Carpenter Lake
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 muc ...
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Bridge River Power Project
The Bridge River Power Project is a hydroelectric power development in the Canadian province of British Columbia, located in the Lillooet Country between Whistler and Lillooet. It harnesses the power of the Bridge River, a tributary of the Fraser, by diverting it through a mountainside to the separate drainage basin of Seton Lake, utilizing a system of three dams, four powerhouses and a canal. Discovery and original development The potential for the project was first observed in 1912 by Geoffrey Downton, a land surveyor, visiting the goldfield towns in the area who noticed the short horizontal distance between the flow of the Bridge River, just above its impressive canyon, and the much-lower Seton Lake. It was fifteen years before this observation was put to task, and not until 1927 that a private company first bored a tunnel through Mission Ridge (also known as Mission Mountain), which separates the basins of the Bridge and Seton systems. This tunnel was completed in 19 ...
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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 ...
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Bend Or
Bend Or (1877–1903) was a British Thoroughbred racehorse who won the 1880 Epsom Derby. His regular jockey Fred Archer, winner of thirteen consecutive British jockey titles, said Bend Or was probably the greatest horse he had ever ridden. Nomenclature His name is the heraldic term for "a bend (i.e. diagonal stripe) that is golden or yellow in color ( or)", and is a reference to the ancient former arms of the Grosvenor family which were adjudged against them in 1389 to the Scrope family in the most famous case ever heard before the Court of Chivalry, known as ''Scrope v Grosvenor''. The Duke also awarded it as a lifelong family nickname to his grandson Hugh Grosvenor, 2nd Duke of Westminster (1879–1953), born in the year before the Derby win. Bendor Range is named after the horse. Breeding Bred and foaled at the 1st Duke of Westminster's Eaton Stud, Bend Or grew to be a large stallion but was noted for his unusual docility. He was a chestnut colt who stood and had a whi ...
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Lillooet, British Columbia
Lillooet () is a district municipality in the Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On BC Highway 99, the locality is by road about northeast of Pemberton, northwest of Lytton, and west of Kamloops. First Nations A main population centre of the Stʼatʼimc (Lillooet Nation), who comprise just over 50 per cent of the Lillooet area residents, it is one of the southernmost communities in North America where indigenous people form the majority. First Nations communities assert the land is traditional territory, having been continuously inhabited for thousands of years. The confluence of several main streams with the Fraser attracted large seasonal and permanent indigenous populations. Situated in the Lower Fountain, the Bridge River Rapids (Sat' or Setl), which blocked migrating salmon, has remained a popular fishing and fish drying site for centuries. Keatley ...
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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 ...
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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 ...
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