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 …

Ecological restoration studies have been widely conducted for many years to solve eco‐
environmental problems. However, no publications offer a systematic and quantitative …

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 …

Geologists frequently debate the origin of iconic river canyons, as well as the extent to which
they record climatic and tectonic signals. Fluvial and hillslope processes work in concert to …

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 …

Large, resistant, quartz‐rich boulders deposited on hillslopes and in channels armour the
landscape, trap sediment and influence hillslope angle and erodibility. In the Virginia …

Sinuous ridges have been interpreted as evidence for ancient rivers on Mars, but relating
ridge geometry to paleo‐hydraulics remains uncertain. Three analog ridge systems from the …

Geomorphologists often rely on simple models of river channel incision for predicting rates
of landscape evolution and channel response to perturbations, as well as extracting climatic …

Earth's terrestrial topography evolves in response to the interaction of tectonics, climate, and
lithology. Recent discoveries suggest that the grain size of sediments produced on hillslopes …

While it is well recognized that vegetation can affect erosion, sediment yield and, over longer
timescales, landform evolution, the nature of this interaction and how it should be modeled is …