We provide field evidence for the role of bedload in driving fluvial incision and knickpoint
propagation. Using aerial photographs, field surveys, and hydrological data, we constrain …

A major control on bedrock incision is the interaction between alluvial cover and erosive
mobile grains. The extent of alluvial cover is typically predicted as a function of relative …

Bedrock channel slope and width are important parameters for setting bedload transport
capacity and for stream-profile inversion to obtain tectonics information. Channel width and …

The advection‐diffusion equation is one of the most widespread equations in physics. It
arises quite often in the context of sediment transport, eg, for describing time and space …

Partial alluvial cover in bedrock channels influences downcutting rates and mountain river
morphodynamics. Flume experiments have demonstrated that a wide range of stable cover …

Models of landscape evolution by river erosion are often either transport-limited (sediment is
always available but may or may not be transportable) or detachment-limited (sediment must …

Rivers are dynamical systems that are thought to evolve towards a steady-state
configuration. Then, geomorphic parameters, such as channel width and slope, are constant …

Wide bedrock valleys and their genetic descendants, strath terraces, can serve as
morphological records of past climate that reflect river discharge and sediment load during …

Depending on their behaviour during extreme floods, streams can be divided into two
distinct classes, which derive from a simple threshold model of transport dynamics.'Flood …

Natural bedrock rivers exhibit diverse erosional morphologies. Although the formation of
alternate bars on bedrock has been noted in previous studies, the influence of these …