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 …

It has long been known that mountain glaciers and continental ice sheets around the globe
reached their respective maximum extent at different times during the last glacial cycle, often …

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 …

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

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 …

The Antarctic Dry Valleys (ADV) are generally classified as a hyper-arid, cold-polar desert.
The region has long been considered an important terrestrial analog for Mars because of its …

Theoretical analysis predicts that enhanced erosion related to late Cenozoic global cooling
can act as a first-order influence on the internal dynamics of mountain building, leading to a …

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