In the most destructive and catastrophic landslide events, rocks, soil and fluids can travel at
speeds approaching several tens of metres per second. However, many landslides …

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 …

Slow‐moving landslides are hydrologically driven. Yet, landslide sensitivity to precipitation,
and in particular, precipitation extremes, is difficult to constrain because landslides occur …

Predicting rainfall‐induced landslide motion is challenging because shallow groundwater
flow is extremely sensitive to the preexisting moisture content in the ground. Here, we use …

Most of the major rivers in the eastern margin of the Tibetan Plateau are distributed along
the tectonic suture zone, where many giant landslides are present. The catastrophic Baige …

Large particles strongly influence flow resistance, energy dissipation, bed stability, and
channel morphology in mountain streams. We conducted flume experiments to evaluate …

Constraining Earth's sediment mass balance over geologic time requires a quantitative
understanding of how landscapes respond to transient tectonic perturbations. However, the …

Boulders are globally widespread and influence processes across many landscapes
including hillslopes, coasts, rivers and extra‐terrestrial settings. Boulders are described as …

Large, rarely mobile boulders are observed globally in mountainous bedrock channels.
Recent studies suggest that high concentrations of boulders could be associated with …

Slow moving landslides regulated by precipitation/snowmelt induced subsurface pore‐
pressure transients can sometimes accelerate to catastrophic failure causing loss of …