Major earthquakes in steep orogens can trigger extensive landsliding. Most of the landslide
bodies come to rest high on the slopes, but subsequent rainfalls can easily remobilize them …

Feedbacks between surface and deep Earth processes in collisional mountain belts depend
on how erosion and topographic relief vary in space and time. One outstanding unknown …

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 …

Bedrock rivers are the pacesetters of landscape evolution in uplifting fluvial landscapes.
Water discharge variability and sediment transport are important factors influencing bedrock …

River channel beds aggrade and incise through time in response to temporal variation in the
upstream supply of water and sediment. However, we lack a thorough understanding of …

The incision rate and steepness of bedrock channels depend on water discharge, uplift rate,
substrate lithology, sediment flux, and bedload size. However, the relative role of these …

The size of grains delivered to rivers by hillslope processes is thought to be a key factor
controlling sediment transport, long-term erosion and the information recorded in …

Structural control on drainage patterns has long been suggested to play an important role in
the development of fluvial systems, including their map pattern. Along the western Taiwan …

Extreme erosion events can produce large short‐term sediment fluxes. Such events
complicate erosion rates estimated from cosmogenic nuclide concentrations in river …

Tropical cyclones (TCs) are an important source of precipitation for much of the eastern
United States. However, our understanding of the spatiotemporal variability of tropical …