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 …

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 …

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 …

Abstract During the Last Glacial Maximum, ice sheets covered large areas in northern
latitudes and global temperatures were significantly lower than today. But few direct …

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 …

Over geologic timescales, CO2 is emitted from the Earth's interior and is removed from the
atmosphere by silicate rock weathering and organic carbon burial. This balance is thought to …

The southern highlands of Mars are dissected by hundreds of valley networks, which are
evidence that water once sculpted the surface. Characterizing the mechanisms of valley …

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 …

Field Techniques in Glaciology and Glacial Geomorphology is the first text to provide this
essential information in a single comprehensive volume. Coverage includes: The role of …

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