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 …

The last glacial maximum (LGM) outline and subsequent retreat pattern (21–7kyr) of North
American ice sheets are reasonably well established. However, the evolution of the ice …

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 …

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 …

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

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 …

We present an 8000‐year history spanning 650 km of ice margin retreat for the largest
marine‐terminating ice stream draining the former British–Irish Ice Sheet. Bayesian …

We present a 10-stage reconstruction of the evolution in ice-flow patterns of the last British
Ice Sheet from build-up to demise derived from geomorphological evidence. 100 flowsets …

Abstract The Last Glacial Maximum (LGM) of Marine Isotope Stage (MIS) 2 is defined here
as the period either of maximum global ice volume or in which major ice sheets reached …

There is a need for fit-for-purpose maps for accurately depicting the types of seabed
substrate and habitat and the properties of the seabed for the benefits of research, resource …