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HYDROLOGICAL REGIME OF LOAD DISCHARGE OF THE RIVERS OF KOLKHETI LOWLAND, GEORGIA
Abstract
The coastal area of the Black Sea of Georgia (Kolkheti Lowland) with its recreational, resort, transport and industrial functions is a very important region in the country. A coastline is formed under the interaction of two environments, the land and the sea with its stability much dependent on the volume and grain size of the coas t-forming material drifted to the coastline by the rivers of the Black Sea basin. 90% of the coastal formations of Georgia belong to an accumulativ e type with their genesis and filled with the alluvium of big rivers (e.g. Enguri, Ri oni). This problem is particularly topical today, if considering that the dynamics of th e river flows, including that of the solid alluvium will have a different reaction on the background of the global warming. Thus, the study of the hydrological regime of the rivers of Kolkheti Lowland and dynamics of the load discharge and evaluation of the mo dern state of anthropogenic impact on it is very important.
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References5
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. Jaoshvili Sh. “The River Alluvium and the Beach Formation of the Georgian Black Sea Coast” Georgia, 1986, pp 78
. Svanidze G. etc. “Kolkheti Lowland – Natural Conditions and Social-Economical aspects” ,Leningrad, 1989, pp 265-273
. Khmaladze G. “Vinosi nanosov rekami chernomorskogo poberezhia Kavkaza”, Gidrometeoisdat, Leningrad, 1978, pp 107-118
. Bilashvili K., Ruso G., Megreli N., Savaneli Z. “D ynamics of the Deltaic Canyon Area, Georgia”. In Book: “Submarine mass movements and their consequences” (3rd Int. Symposium), Springer Publ., vol.27, pp. 251-258, 2007.
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