We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …

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 …

As cosmogenic nuclide applications continue to expand, the need for a common basis for
calculation becomes increasingly important. In order to accurately compare between results …

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 Patagonian glaciations developed from the latest Miocene (c. 6 Ma) in multiple events of
varied duration and intensity. Most of the present glacial landscape is the result of the glacial …

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 …

The most recent maximum in global ice volume occurred around 23,000 to 19,000 years
ago, during Marine Isotope Stage 2 (MIS 2;∼ 29-14 ka) according to benthic δ 18 O and sea …

This paper evaluates the chronology of the last glacial cycle and deglaciation in the Lago
Pueyrredón valley of central Patagonia, 47.5° S, Argentina. The valley was a major outlet of …

The India–Asia collision zone is a key area for understanding continental plateau formation
and mountain building. Two fundamental questions in this context are how the …

Cosmogenic exposure dating of glacial boulders is commonly used to estimate the timing of
past glaciations because the method enables direct dating of the duration a boulder has …