Landscape evolution is controlled by tectonic strain, bedrock lithology, and climatic
conditions, and is expressed in the spatial and temporal variations of river channel networks …

Drainage basins delineate Earth's land surface into individual water collection units. Basin
shape and river sinuosity determine water and sediment dynamics, affecting landscape …

The lateral movement of drainage divides is co-influenced by tectonics, lithology, and
climate and therefore archives a wealth of geologic and climatic information. It also has wide …

Drainage-divide migration, controlled by rock-uplift and rainfall patterns, may play a major
role in the geomorphic evolution of mountain ranges. However, divide-migration rates over …

Normal fault linkage has significant impacts on uplift patterns and erosional processes in
extensional regions. However, geomorphic process-based constraints on landscape …

Landscapes are sculpted by a complex response of surface processes to external forcings,
such as climate and tectonics. Several major river captures have been documented in the …

The structural styles and magnitudes of Alpine tectonic inversion are reviewed for the
Atlantic margin of southwestern (SW) Iberia, a region known for its historical earthquakes …

Erosion rates are widely used to assess tectonic uplift and sediment export from mountain
ranges. However, the scarcity of erosion rate measurements often hinders detailed tectonic …