Abstract
The aim of this article is to clarify the geological structure of the area of interest (in particular the atmospheric water supply area), the assessment of hydrogeological conditions (determination of dominant collectors, flow directions of shallow and deep groundwater flows). From the aspect of the future process of the bordering Vršany quarry, part of the Slatinice dump will be extracted in the future. Since the basic factors that predispose to sliding (slope of the base, the orientation of the base, the character and nature of the deposited soil, etc.) cannot be influenced at the present or in the future, the only way to improve stability of the dump and to minimize the possibility of larger slope deformations, the long-term improvement of the shear contact strength at the interface of the dump with its subsoil.
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