To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …

The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …

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 …

Abstract The Middle and Late Pleistocene glaciations of northern Eurasia had a great impact
on the evolution of the modern drainage system. This paper presents a review and synthesis …

GIS-based reconstructions of Lake Onego development in the Late Pleistocene and the
Holocene are presented. Reconstructions originated from the ideas of the Lake Onego …

The pattern, style, and timing of glaciation of the last Fennoscandian Ice Sheet (FIS) on the
Kola Peninsula and Russian Lapland (northwest Arctic Russia) is widely debated. This is …

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 …

Aeolian sediments and landforms of the former continental ice sheets' periphery can be
used as invaluable sources of information on palaeoenvironmental changes. In the …

ABSTRACT The Severnaya Dvina River valley crosses the former south‐eastern margin of
the last Scandinavian Ice Sheet. Despite a long research history, there remains …

The L ate P leistocene stratigraphy from the S evernaya D vina‐V ychegda region of
northwestern R ussia is revised based on investigations of new localities, revisiting earlier …