Internally generated, or autogenic, terrestrial and marine sediment-transport dynamics can
produce depositional patterns similar to those associated with climatic, tectonic, or sea level …

River incision into bedrock drives the topographic evolution of mountainous terrain and may
link climate, tectonics, and topography over geologic time scales. Despite its importance, the …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …

Geomorphological evidence of incised bedrock channels is widespread in all mountain
landscapes worldwide. However, the processes controlling incision and gorge formation in …

In the future, Earth will be warmer, precipitation events will be more extreme, global mean
sea level will rise, and many arid and semiarid regions will be drier. Human modifications of …

Airborne LiDAR data collected in 1998 and 2009–2010 were used to measure coastal cliff
erosion and retreat between the Mexico/California border and Bodega Head, California. Cliff …

At the largest time and space scales, the pace of erosion and chemical weathering is
determined by tectonic uplift rates. Deviations from equilibrium arise from the transient …

The causes of terrace formation in active orogenic belts have long been studied. Here, we
present a synthesis of 147 available papers on the ages of Quaternary terraces within the …

Investigating rock‐uplift variations in time and space provides insights into the processes
driving mountain‐belt evolution. The Apennine Mountains of Italy underwent substantial …