Lower Campbell Lake | |
---|---|
Coordinates | 50°01′18.3″N125°27′53.3″W / 50.021750°N 125.464806°W |
Primary inflows | Campbell River |
Primary outflows | Campbell River |
First flooded | 1958 |
Surface area | 2,694 ha (6,660 acres) |
Average depth | 17.1 m (56 ft) |
Max. depth | 75.6 m (248 ft) |
Water volume | 458,784,000 m3 (1.62018×1010 cu ft) |
Residence time | 32 days |
Shore length1 | 89.2 km (55.4 mi) |
Surface elevation | 178 m (584 ft) |
References | [1] [2] |
1 Shore length is not a well-defined measure. |
Lower Campbell Lake, also known as Campbell Lake, is a reservoir on Vancouver Island in British Columbia, Canada. The lake is impounded by the Ladore Dam, which was completed in 1958. Resident fish species in the lake include Cutthroat trout, Rainbow trout, Dolly varden, Kokanee salmon, prickly sculpin and threespine stickleback. [2]
Lower Campbell Lake is located approximately 10 kilometres (6.2 mi) west of the city of Campbell River. It makes up the southern portion of the Sayward Forest Canoe Route. The lake has a surface area of 2,694 hectares (6,660 acres) and has a mean depth of 17.1 metres (56 ft), with a maximum depth of 75.6 metres (248 ft).
Its outflow is the Campbell River, which flows in from Upper Campbell Lake through the Strathcona Dam, and out via the Ladore Dam into John Hart Lake. [1] Other tributaries include the Beavertail, Fry, Greenstone and Miller creeks, with water from the Salmon and Quinsam rivers diverted into the lake. Prior to the construction of the dam, Lower Campbell Lake had a surface area of 1,075 metres (3,527 ft). The lake lies in the Coastal Western Hemlock Biogeoclimatic Zone. [2]
The Klamath River flows 257 miles (414 km) through Oregon and northern California in the United States, emptying into the Pacific Ocean. By average discharge, the Klamath is the second largest river in California after the Sacramento River. It drains an extensive watershed of almost 16,000 square miles (41,000 km2) that stretches from the arid country of south-central Oregon to the temperate rainforest of the Pacific coast. Unlike most rivers, the Klamath begins in the high desert and flows toward the mountains – carving its way through the rugged Cascade Range and Klamath Mountains before reaching the sea. The upper basin, today used for farming and ranching, once contained vast freshwater marshes that provided habitat for abundant wildlife, including millions of migratory birds. Most of the lower basin remains wild, with much of it designated wilderness. The watershed is known for this peculiar geography, and the Klamath has been called "a river upside down" by National Geographic magazine.
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Lake Willoughby is a lake in the town of Westmore in Orleans County in the Northeast Kingdom of Vermont, United States.
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Lake Cascade, is a reservoir in the western United States, on the North Fork of the Payette River in Valley County, Idaho. Located in the Boise National Forest, it has a surface area of 47 square miles (122 km2), and is the fourth largest lake or reservoir in the state. The closest cities are Cascade, Donnelly, and McCall, all in the Long Valley of Valley County.
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The Campbell River is a river on Vancouver Island, British Columbia, Canada. It drains into Discovery Passage at the northwest end of the Strait of Georgia at the City of Campbell River. The Kwak'wala name for the river, or for the village near its mouth, at Campbell River Indian Reserve No. 11, is Tla'mataxw. The source of the river is Buttle Lake.
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The Metro Vancouver watersheds, also known as the Greater Vancouver watersheds, supply potable water to approximately 2.7 million residents in the Lower Mainland of British Columbia. They provide tap water to a land area covering more than 2,600 square kilometres (1,000 sq mi), including Vancouver, Langley and Richmond. Metro Vancouver serves a total of 21 member municipalities, one electoral district, and one treaty First Nation. From west to east, the watersheds are the Capilano, the Seymour, and the Coquitlam. They are located in the North Shore Mountains and Coquitlam Mountain, respectively. Each watershed possesses a reservoir for water storage purposes, under the control of Metro Vancouver. The reservoirs are supplied by about 3.5 metres (11 ft) of rain and 4.5 metres (15 ft) of snowpack annually. Two additional off-catchment areas under control of Metro Vancouver contribute to the water supply. The watersheds have a long history of controversies surrounding logging, highway development, and salmon run conservation.
Upper Campbell Lake is a reservoir on Vancouver Island in British Columbia, Canada. The lake was flooded in 1958 for a large hydroelectric project, which raised the water level by 30 metres (98 ft). Crest Creek and headwaters of the Heber River are diverted into the lake. Part of the lake and its watershed is located in Strathcona Provincial Park, and the Strathcona Park Lodge is located on the eastern side. Freshwater fish species in the lake include Cutthroat trout, Rainbow trout and Dolly varden.
John Hart Lake is a reservoir on Vancouver Island in British Columbia, Canada. The lake was created in 1947 when the John Hart Dam impounded the Campbell River, and is the water source for the city of Campbell River. The Campbell River flows from the lake at the John Hart Dam and via the John Hart generating station. The lake has an area of 362.6 ha, with a mean depth of 12.2 metres (40 ft) to a maximum of 22.9 metres (75 ft). The lake is named for John Hart, a Canadian politician who was the 23rd Premier of British Columbia.