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Interest in completing the Columbia Basin Project's 1,100,000 acres (4,500 km 2) has grown in the late 20th and early 21st centuries. One reason for the renewed interest is the substantial depletion of the Odessa aquifer .
The Potholes Reservoir is part of the Columbia Basin Irrigation Project. It is formed by the O'Sullivan Dam and located in central Washington, in the United States. The reservoir is fed by water from Moses Lake, part of the Crab Creek basin. The area features several lakes (typically 30-70 yards wide and 10–30 feet deep).
HAER No. WA-139-I, "Columbia Basin Project, Grand Coulee Switchyards", 7 photos, 29 data pages, 1 photo caption page HAER No. WA-139-J, " Columbia Basin Project, Grand Coulee Construction Towns ", 146 photos, 16 color transparencies, 30 measured drawings, 233 data pages, 9 photo caption pages
According to an economic analysis by Highland Economics the CBDL had done for the project in 2022, the Columbia Basin Project's economic contribution to the country includes $2.66 billion in ...
The Quincy-Columbia Basin Irrigation District (QCBID) is one of three independent non-profit quasi-municipalities founded under Washington state law that hold a contract with the United States Bureau of Reclamation, a division of the United States Department of Interior, to operate and maintain a portion of the Columbia Basin Project.
Hells Canyon Dam, Snake River Snake River near Twin Falls, Idaho Coho Spawning on the Salmon River. The Columbia Basin Initiative is a 2023 agreement between the U.S. government, four sovereign Native American Tribes (Nez Perce, Yakama, Warm Springs and Umatilla) and the U.S. states of Washington and Oregon to provide over $1 billion in funds for salmon restoration and clean energy production. [1]
Banks Lake is a 27-mile-long (43 km) reservoir in central Washington in the United States.. Part of the Columbia Basin Project, Banks Lake occupies the northern portion of the Grand Coulee, a formerly dry coulee near the Columbia River, formed by the Missoula Floods during the Pleistocene epoch.
Pinto Dam and Billy Clapp Lake are part of the Main Canal (1951) of the Columbia Basin project. [8] The canal is 8.3 miles (13.4 km), from Banks lake to Billy Clapp Lake. . From the Billy Clap Lakes outlet, the lower reach of the Main Canal continues westward to divide into the East Low and West Canals near Adco on Washingto