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 …

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 …

Hydrogen usage and storage may contribute to reducing greenhouse gas emissions by
decarbonising heating and transport and by offering significant energy storage to balance …

The new Second Edition of Glacial Geology provides a modern, comprehensive summary of
glacial geology and geomorphology. It is has been thoroughly revised and updated from 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 …

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 …

We present results from a suite of forward transient numerical modelling experiments of the
British and Irish Ice Sheet (BIIS), consisting of Scottish, Welsh and Irish accumulation …

Although erosion of valleys by subglacial meltwater was first proposed more than 100years
ago, the processes that produced these valleys under past ice sheets have remained a topic …