To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …

Geomorphological mapping 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 …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Cosmogenic exposure dating has greatly enhanced our ability to define glacial chronologies
spanning several global cold periods, and glacial boulder exposure ages are now routinely …

The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …

Ice can sculpt extraordinary landscapes, yet the efficacy of, and controls governing, glacial
erosion on geological timescales remain poorly understood and contended, particularly …

Glaciers and ice sheets erode mountains and produce vast quantities of sediments that are
delivered to rivers and oceans, impacting global sediment and biogeochemical balances …

It has long been recognised that the formerly glaciated area of Fennoscandia shows large
spatial differences in thicknesses of Quaternary deposits (mainly tills), and exhibits distinct …

Thirty-eight new cosmogenic (10Be) exposure ages from the Scoresby Sund region of east
Greenland indicate that prominent moraine sets deposited by mountain glaciers date from …