A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …

The ongoing debate about the nature of coupling between climate and tectonics in mountain
ranges derives, in part, from an imperfect understanding of how topography, climate …

Quantitative analysis of digital topographic data is an increasingly important part of many
studies in the geosciences. Initially, performing these analyses was a niche endeavor …

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 …

The highest peaks in Europe are found in the central Greater Caucasus, an orogenic belt
characterized by extremely active tectonic and sedimentary processes. In this rugged …

Sediment grain size links sediment production, weathering, and fining from fractured
bedrock on hillslopes to river incision and landscape relief. Yet models of sediment grain …

Due to the challenges in upscaling daily climatic forcing to geological time, physically
realistic models describing how rainfall drives fluvial erosion are lacking. To bridge this gap …

Landslides are the main source of sediment in most mountain ranges. Rivers then act as
conveyor belts, evacuating landslide-derived sediment. Sediment dynamics are known to …

The evolution of rivers in eroding landscapes plays a key role in determining landscape
relief and modulating climate‐tectonic interactions. A common approach to quantifying river …

Landscape evolution models that invert topography for rock uplift can improve our
understanding of both tectonic and geomorphic processes when properly constrained with …