Proceedings of the 12th International INQUA meeting on paleoseismology, active tectonic and archaeoseismology

of conventional methods is limited when studying active tectonics due to indistinct expressions of tectonics in terrain morphology. To study the effects of Alpine collision on the terrain evolution of the Bohemian Massif, the Novohradské hory Mts. (see Fig. 1) were selected for notable changes in river geometry, well- known bedrock lithology and structural geology. This study focusses onbringingnew morphotectonic and fluvial geomorphology data combined with field structural mapping and sedimentology to better understand the evolution of this relatively stable intraplate area. Fig. 1: Localisation of the study area within Czechia