Result
The geological structure of the area was examined through the drilling of individual engineering-geological wells at intervals of 60-80 meters. These wells, reaching depths of 15 meters, included sampling of rock specimens from both disturbed and undisturbed formations. The network of drilled geological wells, spaced at 60-80 meter intervals, revealed no hazardous underground geological structures in the accessible areas. However, georadiolocation identified several karst formations in a potentially hazardous stage of development.