The limits of fourmajor icesheets can be traced in the present landscape of Poland. Glacial
deposits and ice-dammed lakes indicate a stream-like pattern of advancing ice bodies …

The paper presents the first terrestrial record of millennial-scale palaeo-ice margin
oscillations at the southern fringe of the last Fennoscandian Ice Sheet (FIS) during the last …

This study aims to identify potential geosites and show existing geosites in a young glacial
landscape in northern Poland through a qualitative assessment of the local geoheritage …

The limits of four major ice sheets can be traced in the present landscape of Poland. Glacial
deposits and ice-dammed lakes indicate a stream-like pattern of advancing ice bodies …

A critical verification of the previous stratigraphic Quaternary subdivisions has updated the
setting of the stratigraphic units in Poland. Inconsequently applied classification and …

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 …

This paper presents a comprehensive palaeoenvironmental data set from a trough between
glacial curvilineations (an intra-GCL trough) of the Dobrzyń Lake District, north-central …

Rozwój zlodowaceń w skali globalnej zależy przede wszystkim od warunków klimatycznych,
ale inaczej odbywa się na kontynencie, a inaczej na oceanie. W przypadku oceanu …

North‐central Poland was originally shaped by the Płock lobe of the ice sheet formed during
the Weichselian Glaciation. The majority of the studied area comprises the Dobrzyń …