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Genesis and morphodynamics of the Kamyshevatskaya Spit
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Two stages of the evolution of the Kamyshevatskaya Spit have been identified: the emergence of an accumulative terrace at a relatively low level, followed by the development of the spit bending. In modern conditions, the litho-morphodynamic regime of the spit is characterized by a pulsating process of biogenic sediment supply in both time and space, under conditions of which erosion of the sea coast often occurs. The increase in the distance and its extension into the waters of Yasenskiy Bay was more intense in the 1970-1990s, compared to the 2000s. The situation changed in 2022-2023, when a large volume of sandy shell sediments was deposited along the windward shore.
Title: Genesis and morphodynamics of the Kamyshevatskaya Spit
Description:
Two stages of the evolution of the Kamyshevatskaya Spit have been identified: the emergence of an accumulative terrace at a relatively low level, followed by the development of the spit bending.
In modern conditions, the litho-morphodynamic regime of the spit is characterized by a pulsating process of biogenic sediment supply in both time and space, under conditions of which erosion of the sea coast often occurs.
The increase in the distance and its extension into the waters of Yasenskiy Bay was more intense in the 1970-1990s, compared to the 2000s.
The situation changed in 2022-2023, when a large volume of sandy shell sediments was deposited along the windward shore.
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