Abstract
The bed off the Votkinsk (Kama river) reservoir dam reach is leveling on the whole. Intensive wash out is predominant at low and middle depth. Some bottom elevations were lowered by 1-2 m during 15 years. Material is transported into deep water - more than 6-8 m. Maximum thickness of accumulated deposits reaches up to 5 m, while average values are about 1.1-1.5 m. Facial composition of deposits depends on hydrologic factors: unstable level of reservoir, frequency and strength of storms, ephemeral and perennial currents.
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