Calculations of the stability of the section of the landslide slope of the Odesa coast were performed in the work. The site is located in the Kyiv district of Odessa and is adjacent to the children's health and sports camp "Viktoria". The territory covers the coastal part of the plateau, the terraced slope and the beach area. Artificially created terraces and berms stand out in the relief of the slope, at the foot of the slope in some places a preserved natural beach. The specifics of this area are complex engineering-geological (block structure of the slope, loess subsidence soils) and hydrogeological (several aquifers, high level of groundwater) conditions. Previously, before the implementation of a complex of anti-slide measures, large-scale deep sliding and squeezing landslides took place in this area. The partially implemented engineering protection measures, which consisted in the planning of the slope surface and the arrangement of shore fortifications, did not lead to a complete stabilization of the landslide processes. At the present time, undamped, slow-flowing deformations occur on the landslide slope. These deformations are related to the blocky structure of the slope,
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