Loess deposits in southern Britain contain a record of dust, climate and landscape dynamics
over the last glacial, yet their age and accumulation rate remain poorly known. Furthermore …

The role of Quaternary ice sheet fluctuations in driving meltwater pulses and ocean
circulation perturbations is widely acknowledged. What is less clear is the role 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 …

Initially, terrestrial evidence formed the foundation for the division of Quaternary time.
However, since the 1970s there has been an abandonment of the terrestrial stage …

Predicting the future response of ice sheets to climate warming and rising global sea level is
important but difficult. This is especially so when fast‐flowing glaciers or ice streams …

One of the most important problems in glacial geomorphology is the disagreement regarding
the dates of glacial advances. During the Last Glacial Maximum (LGM,~ 29 to 19 ka), the …

Here we reconstruct the last advance to maximum limits and retreat of the Irish Sea Glacier
(ISG), the only land‐terminating ice lobe of the western British Irish Ice Sheet. A series of …

Shipwrecks are an integral part of our maritime archaeological landscape and are
associated with diverse societal and cultural interests, yielding significant management …

Marine-terminating ice stream behaviour often defines the stability of ice sheets and is
driven by a complex interplay of climatic, oceanic, topographic and glaciological factors …

Understanding the pace and drivers of marine‐based ice‐sheet retreat relies upon the
integration of numerical ice‐sheet models with observations from contemporary polar ice …