СОВРЕМЕННАЯ МОРФОДИНАМИКА БЕРЕГОВОЙ ЗОНЫ КОС «АЗОВСКОГО» ТИПА РАСПОЛОЖЕННЫХ В ПРЕДЕЛАХ УКРАИНЫ

Abstract

Within the northern coast of the Sea of Azov there are some accumulative forms that have similar morphological, morphodynamic and lithodynamic characteristics. These forms of the sea relief united in the group of «azov type» spits. At the present time the investigated accumulative forms develop under conditions of intense erosion. The research carried out by us for the past five years, has shown that erosion of accumulative formsʼ bodies is natural, but the building of the bank protection structures affect the lithodynamic systemʼs integrity and strengthen the process.