This paper presents new results of terrestrial cosmogenic nuclide dating of erratics in
northern Poland. We report the first exposure ages of erratics located on the pre-Local Last …

Abstract The Wda River valley in northern Poland is a polygenetic valley located in a former
subglacial meltwater channel that after ice sheet retreat hosted separate and then …

The Baltic Ice Stream, a large fast‐flowing sector of the last Fennoscandian Ice Sheet that
occupied the present‐day Baltic Sea basin, was first conceptualized in the earliest days of …

Published conceptual models argue that much of the forward motion of modern and ancient
glaciers is accommodated by deformation of soft-sediments within the underlying bed. At a …

The sliding of an ice mass over its bed represents one of the main mechanisms for the
forward motion of glaciers and ice sheets, facilitated by the periodic introduction of meltwater …

Subglacial lakes are common features of contemporary ice masses. However, they are
rarely identified in the geological record. This is due to the difficulty in discriminating …

ABSTRACT The Wissower Bach Syncline on the Jasmund Peninsula (NE Germany) has
been examined to understand the complicated glacitectonic environment in the southern …

During the past decades the effect of glacioisostatic adjustment has received much attention.
However, the response of salt structures to ice-sheet loading and unloading is poorly …

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 macro and microsedimentological data recording subglacial
deformation of a sediment succession at Przeszkoda in north-central Poland under the …