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 …

Efforts to extract information about climate and tectonics from topography commonly assume
that river networks are static. Drainage divides can migrate through time, however, and …

Regional studies of fluvial landforms and long-term (Quaternary) landscape development in
remote mountain landscapes routinely use satellite-derived DEM data sets. The SRTM and …

Evaluating conflicting theories about the influence of mountains on carbon dioxide cycling
and climate requires understanding weathering fluxes from tectonically uplifting landscapes …

In this study, we validate and compare elevation accuracy and geomorphic metrics of
satellite-derived digital elevation models (DEMs) on the southern Central Andean Plateau …

Erosion rates dictate the morphology of landscapes, and therefore quantifying them is a
critical part of many geomorphic studies. Methods to directly measure erosion rates are …

Post‐wildfire changes to hydrologic and geomorphic systems can lead to widespread
sediment redistribution. Understanding how sediment moves through a watershed is crucial …

The extent and persistence of the Earth's soil cover depends on the long-term balance
between soil production and erosion. Higher soil production rates under thinner soils …

Bedrock landslides shape topography and mobilize large volumes of sediment. Yet,
interactions between landslide‐produced sediment and fluvial systems that together govern …

Fluvial landscapes are dissected by channels, and at their upstream termini are channel
heads. Accurate reconstruction of the fluvial domain is fundamental to understanding runoff …