The Last Glacial Maximum (LGM) in Poland is represented by the Leszno Phase and
occurred after 21ka radiocarbon years. In turn the deglacial Poznań Phase is estimated at …

We present a new set of 25 10 Be surface exposure ages of boulders located on the
Pomeranian moraines and of erratic boulders located directly upstream of the Pomeranian …

The concept of widespread, large-strain deformation of subglacial unconsolidated, unfrozen,
sediments during Pleistocene glaciations has inconsistencies in the geological record …

During the Last Glacial Maximum (LGM), the Vistula ice lobe was one of the key
morphological elements at the southern margin of the Scandinavian Ice Sheet in north …

This paper presents a model of end moraine sedimentation based on data from Pleistocene
ice sheet margins. According to this model, end moraines quite often constitute alluvial fans …

Climatically dependent environmental changes and the advance and retreat of glaciers
have controlled the development of sedimentary successions in Denmark during the Middle …

Abstract The Dobrzyń Lakeland (north-central Poland) is characterised by a remarkable
subglacial landscape generated by the last Scandinavian Ice Sheet. This landscape exhibits …

Glacial curvilineations (GCLs) are enigmatic landforms recently discovered in the southern
peripheral area of the last Scandinavian Ice Sheet (SIS). They consist of multiple parallel …

The glacial sediment succession exposed close to the southern margin of the L ate W
eichselian S candinavian I ce S heet in P oland reveals a mosaic consisting of isolated …

This study deals with an issue of thermo-mechanical facies, reflecting specific thermal and
mechanical properties of the subglacial environment. The main objective of this study was to …