We present a new glacier chronology from one of the major end moraine systems of the
Southern Alps. Timing and extent of the Last Glacial Maximum (LGM) advance of the Ticino …

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 …

Modelling experiments of drainage events from proglacial lakes of the Río Baker catchment
(central Patagonia, 46–48 ⁰S) indicate that Atlantic-Pacific drainage reversals may have …

Northern Hemisphere cooling between 1400 and 1900 in the Common Era (CE) resulted in
the expansion of glaciers during a period known as the 'Little Ice Age'(LIA). Early …

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

The left-lateral strike-slip Xianshuihe fault system, located in eastern Tibet, is one of the most
tectonically active intracontinental fault systems in China, if not in the world, along which …

Fresh glacial landforms of the Alpine forelands evidence the presence and extent of large
piedmont glaciers during the Last Glacial Maximum (LGM) and yield valuable insights into …

Distinct moraine complexes are well-preserved at the headwaters of the Requ River valley
on the southern slope of Bujia Gangri, the largest center of modern glaciation in the eastern …

Holocene glacial chronostratigraphies in glaciated valleys spread throughout the Himalayan-
Tibetan orogen, including the Himalaya, Tibet, Pamir, and Tian Shan, are developed using a …

Alpine glacier variations are known to be reliable proxies of Holocene climate. Here, we
present a terrestrial cosmogenic nuclide (TCN)-based glacier chronology relying on 24 new …