We compile detrital 10 Be concentrations of Alpine rivers, representing the denudation rates
pattern for 375 catchments across the entire European Alps. Using a homogeneized …

Mountainous topography reflects an interplay between tectonic uplift, crustal strength, and
climate-conditioned erosion cycles. During glaciations, glacial erosion increases bedrock …

Rockwall erosion in high-alpine glacial environments varies both temporally and spatially.
Where rockwalls flank glaciers, changes in debris supply and supraglacial cover will modify …

The junction of the Dinaric and Hellenic mountain belts hosts a trans-orogenic normal fault
system (Shkoder-Peja Normal Fault, SPNF) that has accommodated oroclinal bending, as …

Denudation of steep rockwalls is driven by rock fall processes of various sizes and
magnitudes. Rockwalls are sensitive to temperature changes mainly because thermo …

Fluvial incision is one of the major erosive processes acting at Earth's surface and is highly
sensitive to tectonic, isostatic and climatic variations. The aim of this study is to distinguish …

Climate change affects the stability and erosion of high‐alpine rock walls above glaciers
(headwalls) that deliver debris to glacier surfaces. Since supraglacial debris in the ablation …

In-situ measurements of soil water content provide important constraints on local/global
hydrology. We demonstrate that the attenuation of the underground flux of cosmic-ray …

Physical weathering in cold, steep bedrock hillslopes occurs at rates that are thought to
depend on temperature, but our ability to quantify the temperature‐dependence of erosion …

Mountains cover about a quarter of the world's land surface, and directly support a
significant proportion of the world's population living within mountainous regions. Mountains …