Earth-surface processes operate across erosionally dominated landscapes and deliver
sediment to depositional systems that can be preserved over a range of timescales. The …

How well do deep-sea sedimentary archives track erosion in upland sources, driven by
climatic change or tectonic forcing? Located on the western edge of South Asian monsoon …

It is widely recognized that collisional mountain belt topography is generated by crustal
thickening and lowered by river bedrock erosion, linking climate and tectonics,,–. However …

Tectonic activity generates topography, and the variability of tectonic forcing is responsible
for topographic patterns and variability of relief in fluvial landscapes. Despite this basic …

Climate, tectonics, and life influence the flux and caliber of sediment transported across
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …

Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

The stream power law model has been widely used to represent erosion by rivers but does
not take into account the role played by sediment in modulating erosion and deposition …

Continental rifting is responsible for the generation of major sedimentary basins, both during
rift inception and during the formation of rifted continental margins. Geophysical and field …

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 …

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 …