The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …

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 …

The present-day great availability of high-resolution Digital Elevation Models has improved
tectonic geomorphology analyses in their methodological aspects and geological meaning …

River research often addresses the influence of anthropogenic and natural processes on the
ecological, hydrological, and geomorphological dynamics of river systems. However, here …

The study of fluvial network rearrangement provides a key to understand past and future
landscape evolution. Large perturbations of hydrographic basins such as the change from …

River capture is a dramatic natural process of internal competition through which
mountainous landscapes evolve and respond to perturbations in tectonics and climate …

The eastern margin of the Tibetan Plateau represents one of the morphologically most active
regions on Earth, where the interplay of recent crustal deformation and subsequent fluvial …

One of the challenges facing Earth Scientists is to determine the extent to which geomorphic
features can be used to extract tectonic signals from landscapes. Here, we quantitatively …

In western Iberia, mechanisms that can explain the transition from endorheic to exorheic
continental-scale drainage reorganization are foreland basin overspill, headwards erosion …

Continental freshwaters are among the most species‐dense ecosystems on Earth, with~ 6%
of all described species compressed into~ 0.8% of the world's surface area and~ 0.01% of …