The cryosphere in mountain regions is rapidly declining, a trend that is expected to
accelerate over the next several decades due to anthropogenic climate change. A cascade …

Integration of regional stratigraphic relationships with data on sediment accumulation,
provenance, paleodrainage, and deformation timing enables a reconstruction of Mesozoic …

Climate influences the erosion processes acting at the Earth's surface. However, the effect of
cooling during the Late Cenozoic era, including the onset of Pliocene–Pleistocene Northern …

The field of (U-Th)/He geochronology and thermochronology has grown enormously over
the past∼ 25 years. The tool is applicable across much of geologic time, new (U-Th)/He …

Abstract The (U-Th)/He dating technique is an essential tool in Earth science research with
diverse thermochronologic, geochronologic, and detrital applications. It is now used in a …

Glacial erosion is fundamental to our understanding of the role of Cenozoic-era climate
change in the development of topography worldwide, yet the factors that control the rate of …

Glacier mass loss is a key contributor to sea-level change,, slope instability in high-mountain
regions, and the changing seasonality and volume of river flow,–. Understanding the …

Glaciers and ice sheets erode mountains and produce vast quantities of sediments that are
delivered to rivers and oceans, impacting global sediment and biogeochemical balances …

By regressing simple, independent variables that describe climate and tectonic processes
against measures of topography and relief of 69 mountain ranges worldwide, we quantify …

Glacial cirques are armchair-shaped erosional hollows, typified by steep headwalls and,
often, overdeepened floors. They reflect former regions of glacier initiation, and their …