Abstract—The article considers the modern dynamics of Bakalskaya Spit (northwestern Crimea), the distal part of which separated in 2010, becoming an island. It is shown that in the last 200 years, the coastline to its east and west has retreated. Analysis of satellite data and geodetic surveys revealed that in the last 30 years, the distal part of the spit shifted northeast by 300 m and the western branch of the spit shifted east by 160 m. After separation of Peschany Island, its area was 0.56 km²; by 2018, it had contracted to 0.31 km². The width of the strait that formed is about 1 km. It has been suggested that an increase in storm activity and an abnormally high Black Sea level in the previous period led to formation of the island under decreased sediment influx conditions.

中文翻译：

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克里米亚海岸新岛的形成

摘要—本文考虑了Bakalskaya Spit（西北克里米亚）的现代动力学，其远端部分于2010年分离，成为一个小岛。结果表明，在过去的200年中，东西向的海岸线逐渐减少。对卫星数据和大地测量的分析表明，在过去30年中，吐痰的远端向东北偏移300 m，吐痰的西分支向东偏移160 m。佩斯基尼岛分离后，面积为0.56 km ²。到2018年，它收缩到0.31 km ²。形成的海峡宽度约为1公里。有人认为，前期风暴活动的增加和异常高的黑海水平导致了在减少泥沙涌入条件下形成岛屿。