Pleistocene periglacial and periglacial-soil structures in the western part of the Holy Cross Mts

Abstract

Rubble festoons developed on tectonically loosened Liassic sandstones are reported from the western part at the Holy Cross Mts, Central Poland. These structures as well as ice-wedge cast and funnel-shaped structures occurring in Quaternary deposits, originated under the periglacial conditions of Pleistocene patchy tundra.