STADY DELTA FORMING PROCESS IN THE MOUTH OF KURA RIVER

The pendent and depth alluvial taking across Kura River are formed as a result of weather process in the basin and river bed. The natural factors climate criterions, soil geological and orphographic condition play an important role in formation of water erosion which has got a special role in weather process.The flow balance influences on qualitative and quantitative change of alluvials of the river water by forming anthropogenic factors as water storehouses and human activity.The measure – observation works over alluvials in the mouth of Kura have been carrying out in Salyan object beginning form 1948. But a study of pendent alluvials in the part where the river delta pours into the sea is begun in the hydrometric object formed in 2 km observation works, pendent alluvial has been studied in the objects activated by intervals in different periods over other tributaries pouring into the sea in the delta

کلیدواژه ها:

alluvial ، Kura River ، weather ، erosion ، qualitative