+Volume 48, 2015 (GRR for 2014) (in print)
Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)
Quaternary geological and palaeopedological investigation near the Zarazice railway station
Geoscience Research Reports 34, 2001 (GRR for 2000),
pages 76–77
Abstract
About 2 thick section trough Quaternary sediments was exposed during the excavation at the Zarazice railway station. Sandy gravel of the "main terrace" of the Morava River (Middle Pleistocene) is overlain by a bed of soil sediment disturbed by typical frost-wedge casts, evidencing the existence of fossil permafrost. The top part of the section is represented by the youngest loess with topsoil developed on its surface.