Determination of the spatial position of the boundaries in the plan and tectonic discontinuities, karst voids, identification of water-saturated rocks at depths of up to 70 m along the sides of the quarry.
Result
Extended zones of increased conductivity were identified - probably increased humidity at depths of 8-25 m.
Areas characteristic of fracture zones were found.
Value
Prompt acquisition of information about the state of the sides of quarries: the presence of moisture-saturated areas, places of karst formation, fracture zones.
