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 …

The record of ice-sheet demise since the last glacial maximum (LGM) provides an
opportunity to test the relative importance of instability mechanisms, including relative sea …

The findings of BRITICE‐CHRONO Transect 2 through the North Sea Basin and eastern
England are reported. We define ice‐sheet marginal oscillation between~ 31 and 16 ka, with …

The record of the confluence and collapse of the British‐Irish Ice Sheet and the
Fennoscandian Ice Sheet is obscured by the North Sea, hindering reconstructions of the …

The glacial evolution of western Cumbria, England is reassessed following a
comprehensive review of both published and extensive unpublished records from the …

The climatic transition from the Last Glacial Maximum (LGM) to the early Holocene (ca. 18–
12 ka BP) involved rates of temperature change comparable with present-day warming …

Both modern and palaeo‐ice streams experience shutdown, which has critical implications
for their mass balance and influence on relative sea level. Reconstructions of palaeo‐ice …

This paper presents new sedimentological, geomorphological, and optically stimulated
luminescence (OSL) geochronological evidence for fluvial evolution of the mid-to lower …

Abstract Investigations at Pepper Arden Bottoms, a lake basin site on the interfluve between
the rivers Tees and Swale in northeast England, have recovered lithostratigraphical, pollen …

Rapid earth surface evolution is discrete in nature, with short‐duration extreme events
having a widespread impact on landscapes despite occurring relatively infrequently. Here …