Abstract The Yellow River Basin (YRB) is characterized by active geological and tectonic
processes, rapid geomorphological evolution, and distinct climatic diversity …

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 …

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

Bedrock landslides shape topography and mobilize large volumes of sediment. Yet,
interactions between landslide‐produced sediment and fluvial systems that together govern …

Although the general concept that escarpments in layered rocks retreat through time was
offered more than 150 years ago, recognizing the exact mechanisms, patterns and rates of …

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 …

Coarse clastic sedimentary successions cover approximately-one fourth of the continental
surface and give rise to distinctive landforms at a variety of scales. Rock-mass strength …

Computational modeling occupies a unique niche in Earth and environmental sciences.
Models serve not just as scientific technology and infrastructure but also as digital containers …

We present new geochronological data derived from hillslope boulder armor in the Flint Hills
in northeastern KS, United States, that provides insights into the rates and timing of lateral …

Mechanical weathering comprises the physical breakdown of rock that occurs upon
reaching Earth's surface. There, the ongoing evolution and interactions of topography …