— — the river that turns around at the top.
“The Columbia begins quietly, in a long shallow lake at the south end of British Columbia's Rocky Mountain Trench. It runs north for almost five hundred kilometres before reversing course at the Big Bend and heading south for the United States. Along the way it gathers Kinbasket Lake, the Mica reservoir, and the long arm above Revelstoke. The Selkirks rise on one side, the Rockies on the other.
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The Columbia River rises at Columbia Lake in the southern Rocky Mountain Trench of British Columbia, at roughly 820 m elevation. From source to mouth at Astoria, Oregon, it runs about 2,000 km and drains 670,000 km² across seven U.S. states and one Canadian province. The Canadian reach covers the upper 801 km, flowing north along the Trench to the Big Bend, then south through the Selkirk Mountains and past Revelstoke before crossing the international border below Castlegar into Washington State.
Three large dams shape the Canadian Columbia. Mica Dam, completed in 1973, holds back Kinbasket Lake and stands 243 m high, one of the tallest earthfill dams in the world. Revelstoke Dam, completed in 1984, sits downstream and feeds the seven-unit Revelstoke Generating Station. Hugh Keenleyside Dam, completed in 1968 above Castlegar, regulates flow across the border under the Columbia River Treaty between Canada and the United States. Together they produce roughly half of British Columbia's electricity.
The Canadian Columbia is open most of the year. The headwater lakes and the long reservoirs freeze along their margins from December through March but rarely close completely. The water runs cleanest and bluest in late summer, August through September, after the Selkirk snowmelt has settled. The road along the Big Bend, Highway 23 north from Revelstoke, runs only as far as Mica Creek and is plowed in winter to the dam. Beyond that point the basin holds only the river, the lakes, and the line of the Trench.