Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

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 …

In meandering rivers cut into bedrock, erosion across a channel cross‐section can be
strongly asymmetric. At a meander apex, deep undercutting of the outer bank can result in …

We present an experimental analysis of hydraulic roughness variations due to changes in
alluvial cover in a mixed bedrock-alluvial meandering channel with larger bedrock …

Several studies have demonstrated the importance of alluvial cover; furthermore, several
mathematical models have also been introduced to predict the alluvial cover on bedrock …

Successful management of natural and engineered channels with discontinuous alluvial
cover requires knowledge of how the cover develops and evolves. We report on physical …

Mixed bedrock‐alluvial rivers can exhibit partial alluvial cover, which plays an important role
in controlling bedrock erosion rates and landscape evolution. However, numerical …

Previous research into sediment cover in bedrock‐alluvial channels has focussed on total
sediment cover, rather than the spatial distribution of cover within the channel. The latter is …

The alluvial cover in channels with non‐alluvial beds is a major morphologic feature in these
rivers and has important geomorphic and ecologic functions. Although controls on the extent …

In bedrock rivers, erosion by abrasion is driven by sediment particles that strike bare
bedrock while traveling downstream with the flow. If the sediment particles settle and form an …