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Bridge River
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Bridge River
The Bridge River is a river in southern British Columbia, Canada. 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 most of the river's 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.
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 men. The river came to be called the Bridge River due to the location of a bridge across the Fraser at this point, originally a pole-structure built by the native St'at'imc people but replaced at the time of the Fraser Canyon Gold Rush in 1858 by a settler-run tollbridge. The Bridge River Ocean, an ancient ocean, takes its name from the Bridge River.
The 142-kilometre (88 mi) long river drains a region of 4,660 square kilometres (1,800 sq mi) in the Pacific Range, a sub-range of the Coast Mountains of southeastern British Columbia. Its source is the Bridge Glacier, which is part of the larger Lilloet Icefield. The Upper Bridge River, which flows from the Bridge Glacier to Downton Lake, is the only free-flowing section of the river. Downton Lake is a reservoir formed from the Lajoie Dam, the first of three dams in the Bridge River Power Project. A short outflow after the dam meets the Hurley River, and then flows into another reservoir, Carpenter Lake. This 40-km long lake is impounded by Terzaghi Dam. Near the dam, tunnels through Mission Mountain divert much of the river's waters underground to Seton Lake to facilitate power generation.
Below Terzaghi Dam, the mostly dry riverbed runs through the immense gorge of the Bridge River Canyon. The river is joined by the Yalakom River near Horseshoe Canyon and the community of Moha.
Its confluence with the Fraser occurs at a double gorge formed by the two rivers, which are forced through narrow banks at this point and reminiscent of a fountain, near today's community of Fountain.
The Yalakom, whose name means 'the ewe of the mountain sheep' in the Chilcotin language, was formerly known as the North Fork of the Bridge and now provides much of the flow for the river below the diversion at Carpenter Lake. The South Fork of the Bridge River is many miles upstream, at the community of Gold Bridge, and is today known as the Hurley River (originally Hamilton's River). Several other large feeder streams contribute to the diverted flow of the Bridge, including Gun Creek, Tyaughton Creek, Marshall Creek, and Cadwallader Creek; the last-named is a tributary of the Hurley, about 15 kilometres upstream from its confluence with the Bridge.
From 1961 until 2000, the Lower Bridge River between Terzaghi Dam and the confluence with the Yalakom was almost completely dry due to water diversion. Before the dam was constructed, the mean streamflow in this stretch was 100 square metres (1,100 sq ft) per second. In 2000, BC Hydro began restoring a small, regular flow, with seasonal adjustments to mimic natural fluctuations. The mean flow of the lower Bridge below the dam is now 3 square metres (32 sq ft) per second, and riparian vegetation has recovered somewhat in that section.
Due to the force of the rivers at the Bridge's original confluence into the Fraser, the area has been for millennia the most important inland salmon-fishing site on the Fraser. The flow of the Bridge River, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project in 1961, with the water now entering the Fraser River just south of Lillooet as a result. The salmon fishery of the Bridge River was near-entirely destroyed by this diversion.
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Bridge River
The Bridge River is a river in southern British Columbia, Canada. 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 most of the river's 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.
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 men. The river came to be called the Bridge River due to the location of a bridge across the Fraser at this point, originally a pole-structure built by the native St'at'imc people but replaced at the time of the Fraser Canyon Gold Rush in 1858 by a settler-run tollbridge. The Bridge River Ocean, an ancient ocean, takes its name from the Bridge River.
The 142-kilometre (88 mi) long river drains a region of 4,660 square kilometres (1,800 sq mi) in the Pacific Range, a sub-range of the Coast Mountains of southeastern British Columbia. Its source is the Bridge Glacier, which is part of the larger Lilloet Icefield. The Upper Bridge River, which flows from the Bridge Glacier to Downton Lake, is the only free-flowing section of the river. Downton Lake is a reservoir formed from the Lajoie Dam, the first of three dams in the Bridge River Power Project. A short outflow after the dam meets the Hurley River, and then flows into another reservoir, Carpenter Lake. This 40-km long lake is impounded by Terzaghi Dam. Near the dam, tunnels through Mission Mountain divert much of the river's waters underground to Seton Lake to facilitate power generation.
Below Terzaghi Dam, the mostly dry riverbed runs through the immense gorge of the Bridge River Canyon. The river is joined by the Yalakom River near Horseshoe Canyon and the community of Moha.
Its confluence with the Fraser occurs at a double gorge formed by the two rivers, which are forced through narrow banks at this point and reminiscent of a fountain, near today's community of Fountain.
The Yalakom, whose name means 'the ewe of the mountain sheep' in the Chilcotin language, was formerly known as the North Fork of the Bridge and now provides much of the flow for the river below the diversion at Carpenter Lake. The South Fork of the Bridge River is many miles upstream, at the community of Gold Bridge, and is today known as the Hurley River (originally Hamilton's River). Several other large feeder streams contribute to the diverted flow of the Bridge, including Gun Creek, Tyaughton Creek, Marshall Creek, and Cadwallader Creek; the last-named is a tributary of the Hurley, about 15 kilometres upstream from its confluence with the Bridge.
From 1961 until 2000, the Lower Bridge River between Terzaghi Dam and the confluence with the Yalakom was almost completely dry due to water diversion. Before the dam was constructed, the mean streamflow in this stretch was 100 square metres (1,100 sq ft) per second. In 2000, BC Hydro began restoring a small, regular flow, with seasonal adjustments to mimic natural fluctuations. The mean flow of the lower Bridge below the dam is now 3 square metres (32 sq ft) per second, and riparian vegetation has recovered somewhat in that section.
Due to the force of the rivers at the Bridge's original confluence into the Fraser, the area has been for millennia the most important inland salmon-fishing site on the Fraser. The flow of the Bridge River, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project in 1961, with the water now entering the Fraser River just south of Lillooet as a result. The salmon fishery of the Bridge River was near-entirely destroyed by this diversion.
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