New data have been obtained on the time of isolation from the sea of three lake located at altitudes of 13.8, 34.6 and 65.2 m above sea level in the Dalnie Zelentsy. Based on new data and revision of already known data, a new graph of the sea level change was constructed. It was determined that at the end of the Pleistocene and the beginning of the Holocene, the land was rapidly uplifted at a rate of up to 25 mm/year. Then, for more than 3000 years, the sea level has been at the same altitude for a long time, or a slight rise in sea level could occur. Over the past 7000 years, there was a gradual uplift of the land at a rate of about 2–3 mm/year.
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Толстобров et al. (2024) studied this question.
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