Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

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 …

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 …

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 …

Understanding the evolution of the ice-bed interface is fundamentally important for gaining
insight into the dynamics of ice masses and how subglacial landforms are created. However …

Ice sheets reshape Earth's surface. Maps of the landscape formed by past ice sheets are our
best tool for reconstructing historic ice sheet behavior. But models of glacier erosion and …

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 …

Subglacial bedforms are a range of landforms (10-105m long) shaped mostly in glacial
sediments and are abundant on ice-sheet beds. Numerous explanations for their …

At present, there remains uncertainty surrounding the glacial history of the Fennoscandian
Ice Sheet on the Kola Peninsula and Russian Lapland, northwest Arctic Russia. This is …

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 …