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 …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …

Map** and forty-seven new 10 Be ages help define the timing of glaciation in the Ladakh
and Pangong Ranges in Northwest India. Five new local glacial stages are defined for the …

Surface exposure dating using cosmic-ray-produced nuclides has been applied to
determine the age of thousands of landforms produced by alpine glaciers in mountain areas …

Determining whether glaciers registered the classic Last Glacial Maximum (LGM;∼ 26,500–
∼ 19,000 yrs ago) coevally between the hemispheres can help to discriminate among …

Schmidt-hammer exposure-age dating (SHD) is a numerical, calibrated-age dating
technique based on the degree of weathering of rock surfaces. The Schmidt hammer …

Glaciers offer the potential to reconstruct past climate over timescales from decades to
millennia. They are found on nearly every continent, and at the Last Glacial Maximum …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

Temperate glaciers are very sensitive to changes in the global climate system and provide
an excellent opportunity to obtain information on the timing and magnitude of palaeoclimatic …

While revolutionary to the geomorphic community, the application of terrestrial cosmogenic
nuclide (TCN) dating is complicated by geological uncertainties, which often lead to skewed …