▪ Abstract Avulsion is the natural process by which flow diverts out of an established river
channel into a new permanent course on the adjacent floodplain. Avulsions are primarily …

Anastomosing rivers constitute an important category of multi-channel rivers on alluvial
plains. Most often they seem to form under relatively low-energetic conditions near a (local) …

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

The three-dimensional geometry of fluvial channel bodies and valley fills has received much
less attention than their internal structure, despite the fact that many subsurface analyses …

Many of the world's extensive warm dryland regions support numerous, albeit often
infrequently flowing, rivers. Dryland rivers are increasingly a focus of scientific and applied …

River-wetland corridors form where a high degree of connectivity between the surface
(rheic) and subsurface (hyporheic) components of streamflow creates an interconnected …

Fluvial landscapes diversified markedly over the 250 million years between the Cambrian
and Pennsylvanian periods. The diversification occurred in tandem with the evolution of …

Many Australian inland rivers are characterised by vast floodplains with a network of
anastomosing channels that interconnect only during unpredictable flooding. For much of …

It is often taken for granted that rivers organize transport into a single active channel. In
some net-depositional environments, however, flow of water and sediment is distributed in …

River avulsions are commonly considered to be driven by the aggradation and growth of
alluvial ridges, and the associated increase in crossvalley slope relative to either the down …