Abstract
A general characteristics is made of the set of anti-landslide measures at the Odessa sea coast. Based on multi-year regime observations over the operational efficiency of anti-landslide constructions, it is shown that the modern geodynamics of landslide slopes is determined by the combination and relationships of various factors. The most important factors are: micro-block structure of the plateau edge and landside slopes, high sensitivity, mobility and changeability of properties of the geological environment.
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