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Sediment Transport in the Lower Snake and Clearwater River Basins, Idaho and Washington, 2008?11 (in English)
Ryan L. Fosness
(Author)
·
Molly S. River
(Author)
·
Gregory M. Clark
(Author)
·
Createspace Independent Publishing Platform
· Paperback
Sediment Transport in the Lower Snake and Clearwater River Basins, Idaho and Washington, 2008?11 (in English) - Fosness, Ryan L. ; River, Molly S. ; Clark, Gregory M.
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Synopsis "Sediment Transport in the Lower Snake and Clearwater River Basins, Idaho and Washington, 2008?11 (in English)"
Sedimentation is an ongoing maintenance problem for reservoirs, limiting reservoir storage capacity and navigation. Because Lower Granite Reservoir in Washington is the most upstream of the four U.S. Army Corps of Engineers reservoirs on the lower Snake River, it receives and retains the largest amount of sediment. In 2008, in cooperation with the U.S. Army Corps of Engineers, the U.S. Geological Survey began a study to quantify sediment transport to Lower Granite Reservoir. Samples of suspended sediment and bedload were collected from streamgaging stations on the Snake River near Anatone, Washington, and the Clearwater River at Spalding, Idaho.