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 …

The evolution and dynamics of the last British–Irish Ice Sheet (BIIS) have hitherto largely
been reconstructed from onshore and shallow marine glacial geological and …

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 …

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 …

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 …

Cosmogenic exposure dating has greatly enhanced our ability to define glacial chronologies
spanning several global cold periods, and glacial boulder exposure ages are now routinely …

The last decade has seen a global surge in the number and resolution of well-dated
geomorphological reconstructions of mountain glacier fluctuations and former ice sheet …

Cosmogenic exposure dating of glacial boulders is commonly used to estimate the timing of
past glaciations because the method enables direct dating of the duration a boulder has …

The ice sheet that once covered Ireland has a long history of investigation. Much prior work
focussed on localised evidence-based reconstructions and ice-marginal dynamics and …

Global climate changes during the Quaternary reveal much about broader evolutionary
effects of environmental change. Detailed regional studies reveal how evolutionary lineages …