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The modern geomorphological appearance of the northern coast of the Sea of Azov was formed during the last 2 thousand years under the conditions of modern neotectonics, intensive hydrodynamic regime, and abrasion and accumulative processes. At the same time, most of the accumulative forms of the North Pryazovia region – sea spits – were formed. In geomorphological terms, the spits of the northern coast of the Sea of Azov are lowlands, in the form of sandy and shell peninsulas, which wedge deeply into the water are...