During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …

We present a conceptual model for the deglaciation of Atlantic Canada in which a role is
played by ice streams. The ice margin lay close to the edge of the continental shelf at the last …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Morphological interpretation of regional and detailed bathymetric data sets on the 2500-km-
long Norwegian shelf from the North Sea (57° N) to Svalbard (80° N) has revealed a …

The detailed mapping of the Storegga Slide morphological elements and the analyses of the
slide development are based on high-quality acoustic and sampling data sets acquired …

Strongly divided opinion has led to competing, apparently contradictory, views on the timing,
extent, flow configuration and decay mechanism of the last British Ice Sheet. We review the …

Twelve palaeogeographical reconstructions illustrate environmental changes at the
southwest rim of the Scandinavian Ice Sheet 40–15 kyr BP. Synchronised land, sea and …

In this paper new and previously published data on the Pleistocene glacial impact on the
NW European margin from Ireland to Svalbard (between c. 48° N–80° N) are compiled. The …

Marine and terrestrial datasets (swath bathymetry, 2D and 3D seismic and remote sensing
data) are used to map the megascale glacial geomorphology of the southern Barents Sea …

Ice streams influence ice sheet mass balance and stability but key aspects of their behaviour
remain poorly understood. This paper reviews and discusses one very important aspect …