Area of old hard rocks ; Bohemia ; Czech Republic ; Fluvial terrace ; Geomorphology ; Morphostratigraphy ; Quaternary ; Stream
The results of geomorphological research into the Sázava river terraces are presented. This terrace system is characteristic by its variable structure which is conditioned by specific hydrodynamic processes that existed during the late Cenozoic
This article presents the results of a geomorphological analysis of localities of Quaternary river terraces along the Želivka River and its historical-genetic interpretation in light of the formation of the Sázava terrace system. In addition