Hydrologický režim v sesuvném území Gírová

Abstract

In this thesis i I am deal with the main causes of slope movement activation on the southern slope of Gírová Mountain. In the first part I am characterize natural conditions from the geological, geomorphological, hydrogeological, geomorphological, tectonic and climatic point of view. In the second part I am characterized the slope movements. The next section contains methods and measurement results that have been conducted and evaluated by scientists to determine the main parameters of slope movement activation. In the last part of this work I am dealt with the emergence and significance of lanslide dams, which originated in the landslide.