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During the period 1972-79,~load0 in the Clearwater River ranged from about 50,000 tons (45,000 metric tons) per year in 1972 and 1974 to about 1,000 tons (910 metric tons) per year in the drought years of 1973 and 1977. Suspendedsediment load at the same location ranged from about 1,000,000 tons (910,000 metric tons) per year to about 50,000 tons (45,000 metric tons) per year for the same respective years. In the Snake River, bedload ranged from about 200,000 tons (180,000 metric tons) per year for 1972 and 1974 to about 10,000 tons (9,100 metric tons) per year in 1973; bedload was too low for determination in 1977. Suspendedsediment load ranged from about 5,000,000 tons (4,500,000 metric tons) per year in 1974 to about 50,000 tons (45,000 metric tons) per year in 1977. » edload thus ranged from about 2 to 10 percent of suspended load and averaged about 5 percent. For either river, bedload particle size was bimodal. Modes were in the mediumto coarse-sand range and in the very coarse-gravel range. Suspended-sediment_£article size was generally finer than sand.

Sediment transport in the Snake and Clearwater rivers in the vicinity of Lewiston, Idaho