Deglaciation ; Fluvioglacial features ; Glacial features ; Glacial tectonics ; Microstructure ; Moraine ; Petrology ; Poland ; Terminology
Based on research results obtained in west central Poland, the aim of this paper is to discuss in brief the existing terms and to propose a new terminology. It is oriented towards genetic and petrologic criteria, adapted for unconsolidated deposits
, suggesting a re-advance. Petrological data suggest also a change of ice flow direction from north-south during the major advance to northeast-southwest during the readvance. Thus now, almost all marginal zones of the Late Weichselian glaciation in western