затоплення

Aim of this research is to determine the area of land flooding according to a reasonably chosen hydrological model for a complex section of the Dniester River at the place of transition from the foothill to the plain with complex meandering and significant shifts of the river. Methods. The method of investigation of flooded areas as a result of water rise to a certain level has been processed.

On the basis of geodesic pretentious novelties the transversal types of river-bed are built r. Stryj, nearbyс. Stryj. The analysis of results of supervisions is given by possibility to draw conclusion about the processes of transfer and accumulation gravel the masses in a river-bed and lower lyinga valley Stryj.