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 …

Our understanding of how global climatic changes are translated into ice-sheet fluctuations
and sea-level change is currently limited by a lack of knowledge of the configuration of ice …

The evolution of past global ice sheets is highly uncertain. One example is the missing ice
problem during the Last Glacial Maximum (LGM, 26 000-19 000 years before present)–an …

The European Alps, the cradle of pioneering glacial studies, are one of the regions where
geological markers of past glaciations are most abundant and well-studied. Such conditions …

" Sometime before 15,000 years ago, a band of hunter-gatherers arrived in Northeast Asia.
They continued east, becoming the first people to set foot in the Americas. They soon found …

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 …

Abstract The Laurentide Ice Sheet was the largest global ice mass to grow and decay during
the last glacial cycle (~ 115 ka to~ 10 ka). Despite its importance for driving major changes …

This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new mapping inventory that includes previously hypothesised ice …

While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …