An erodible bed sheared by a fluid flow, gas or liquid, is generally unstable, and bed forms
grow. This review discusses the following issues, in light of the recent literature: What are the …

The use of sedimentary structures as indicators of flow and sediment morphodynamics in
ancient sediments lies at the very heart of sedimentology, and allows reconstruction of …

Submarine sediment density flows are one of the most important processes for moving
sediment across our planet, yet they are extremely difficult to monitor directly. The speed of …

Sedimentary rocks contain the most important archive of environmental change through
earth history. They record changing climates, the movement of plates, and the rise and fall of …

Rivers and Floodplains is concerned with the origin, geometry, water flow, sediment
transport, erosion and deposition associated with modern alluvial rivers and floodplains …

Sediment fluxes in aquatic environments are crucially dependent on bedform dynamics.
However, sediment-flux predictions rely almost completely on clean-sand studies, despite …

Flows with high suspended sediment concentrations are common in many sedimentary
environments, and their flow properties may show a transitional behaviour between fully …

Most past studies of river dune dynamics have concentrated on two‐dimensional (2‐D) bed
forms, with constant heights and straight crest lines transverse to the flow, and their …

Turbidity currents are notoriously difficult to monitor directly, therefore interpretation of their
deposits forms the basis for much of our understanding of these flows. The deceleration rate …

River Processes deals primarily with flow and sediment dynamics in alluvial channels. It
emphasises water flows (basic principles and characterisation), fluvial sediment, processes …