The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

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

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 …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …

Geomorphological mapping is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …

During the last glaciation, most of the British Isles and the surrounding continental shelf were
covered by the British–Irish Ice Sheet (BIIS). An earlier compilation from the existing …

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 …