Quaternary sediments on the map sheet area 11-424 Dolní Bělá

 

Oldřich Holásek

Geoscience Research Reports 40, 2007 (GRR for 2006), pages 64–66
Map sheets: Manětín (11-42)

Full text (PDF, 0.21 MB)

 

Abstract

Quaternary sediments are present in extremely small extent as denudation processes prevailed. Holocene sediments of fluvial and run-off origin fill valleys and depressions in recent morphology, organic and colluvial sediments were found in limited extent and thickness. Upper Pleistocene aeolian and colluvial deposits are present very rarely. Accumulations of anthropogene deposits (pit tips) in places of previous mining activities are present.