Quaternary sediments on the map sheet 22-221 Sedlčany
Geoscience Research Reports 37, 2004 (GRR for 2003),
pages 57–58
Abstract
The area was affected with denudation processes during the Quaternary and sediments are extended in rather small scale. Colluvial sediments with aeolian admixture in places are of the most importance reaching the maximal thickness of 21 m. Colluvio-fluvial and fluvial sediments fill a network of valleys and slope depressions.