▪ 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) …

In an earlier book, The Geology of Fluvial Deposits (1996), I set out in detail modern
methods of facies and architectural analysis of fluvial deposits, and used numerous case …

Alluvial deposits of the Guadalope-Matarranya system (Oligocene, Ebro basin, Spain) and
the Wasatch Formation (Eocene, western Colorado), provide time-integrated records of the …

Recent development of fluvial facies models has been due to improved description of
natural river and floodplain processes and deposits using:(1) ground-penetrating radar …

Channel fills are common elements of Holocene river systems and older fluvial sequences,
but surprisingly little is known about formation and their sedimentary build‐up. Abandoned …

Rivers self-organize their pattern/planform through feedbacks between bars, channels,
floodplain and vegetation, which emerge as a result of the basic spatial sorting process of …

At river bifurcations, water and sediment are divided over two branches. The dynamics of the
bifurcation determine the long‐term evolution (centuries) of the downstream branches …

There is as yet no rational basis for predicting the conditions leading to avulsion of a
meandering river. Here we present a conceptual model and quantify it under simplifying …

Although researchers now recognize that Indigenous knowledge can strengthen
environmental planning and assessment, little research has empirically demonstrated how …