ЛАНДШАФТНАЯ СТРУКТУРА ЗАПАДНОГО ПРИБРЕЖЬЯ ГОРОДА СЕВАСТОПОЛЯ

Abstract

The information about the landscape structure of the western coast of Sevastopol. Landscape studies (summer 2020) were conducted by detailed study of key sites using landscape profiling. In the landscape structure of the study area identified 8 bottom natural complexes (BCN). The capes at a depth of 0.5-5 m are characterized by underwater slope landscapes with boulder and boulder heaps and bedrock outcrops dominated by Carpodesmia crinita and Treptacantha barbata. Between the capes at these depths, underwater slope landscapes formed by sandy sediments, devoid of benthic vegetation, where individual clumps are also dominated by Carpodesmia crinita and Treptacantha barbata. An underwater coastal slope composed of coarse-clastic sediments dominated by Treptacantha barbata, and with alternating pebble-gravel with battered shell sediments dominated by Phyllophora crispa, was recorded at a depth of 5–10 m. A weakly sloping plain composed of gravel-sandy sediments with broken shells, dominated by Phyllophora crispa, can be traced at a depth of 10–15 m. The formation of its landscape structure is influenced by both the natural features of the coastal zone and economic activities in the adjacent territory.