Scandinavian Ice Sheet, one of the largest Pleistocene glacial masses, covering most of northern Europe. (The Pleistocene Epoch began about 2,600,000 years ago and ended about 11,700 years …

Map showing the extent of the Scandinavian, Barents-Kara and British Ice Sheets during two periods. Full line shows the Saalian glaciation and stippled line the Late Weichselian glaciation. (Modified …

The Fennoscandian Ice Sheet of the Weichselian glaciation most likely grew out of a mountain glaciation of small ice fields and ice caps in the Scandinavian Mountains.

The Scandinavian Ice Sheet (SIS), the centre of which was situated in the Scandinavian mountain range, covered Finland and the NW Russian Plain several times during the Quaternary cold stages.

2 days ago · The extent and speed of ice moving off the ice sheets of Greenland and Antarctica into the sea – an important dynamic for climate and sea-rise modelling – has been captured over a 10-year …

This paper explores the glacial history of Gaustatoppen Mountain in southern Norway using cosmogenic nuclide analysis (in situ ¹⁴C, ²⁶Al, ¹⁰Be, ²¹Ne) from a vertical transect of surface samples and a …

The ice sheet originated from the Jostedalsbreen area in Norway and spread to Great Britain on the west, central Germany and Poland on the south, and nearly to Moscow on the east.

We present a new time-slice reconstruction of the Eurasian ice sheets (British–Irish, Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …

Apr 5, 2024 · Abstract. The Scandinavian topography and bathymetry have been shaped by ice through numerous glacial cycles in the Quaternary. In this study, we investigate how the changing …

An ice-cap which developed over Scandinavia during the Quaternary. It has been suggested, largely on the basis of the degree of downwarp and the partial recovery of the land surface in Scandinavia and …