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 …

The pattern, style, and timing of glaciation of the last Fennoscandian Ice Sheet (FIS) on the
Kola Peninsula and Russian Lapland (northwest Arctic Russia) is widely debated. This is …

The last Scottish Ice Sheet (SIS) expanded from a pre-existing ice cap after∼ 35 ka.
Highland ice dominated, with subsequent build-up of a Southern Uplands ice mass. The …

Abstract The southern North Sea is a particularly important area for understanding the
behaviour of the British-Irish Ice Sheet (BIIS) during the last glacial cycle. It preserves a …

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 …

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 …

We present a new chronology to constrain ice‐margin retreat in the northern Irish Sea Basin.
Estimates on the timing of ice thinning derived from surface exposure ages for boulders from …

Ninety-eight surfaces related to the retreat of the British Ice Sheet (BIS) and dated using
Terrestrial Cosmogenic Nuclide Dating (TCND) were sampled using the Schmidt Hammer to …

Abstract During the Last Glacial Maximum, the Vale of York and North Sea lobes of the
British and Irish Ice Sheet extended to within 10 km of each other, impounding a series of …

Abstract During the Last Glacial Maximum (LGM), ice streams of the last British-Irish Ice
Sheet (BIIS) controlled ice discharge from various dispersal centres. Deglaciation was …