Clinoforms are inclined and normally basinward-dipping horizons developed over a range
of spatial and temporal scales in both siliciclastic and carbonatic systems. The study of …

Fluvial landforms and deposits provide one of the most readily studied Quaternary
continental records, and alluvial strata represent an important component in most ancient …

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 …

▪ 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 …

The major goal of this book is to bring together evidence of active deformation on alluvial
rivers, with emphasis on geomorphological adjustment. The authors have grouped their …

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) …

A series of laboratory experiments demonstrates that riparian vegetation can cause a
braided channel to self‐organize to, and maintain, a dynamic, single‐thread channel. The …

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

River bifurcations are critical but poorly understood elements of many geomorphological
systems. They are integral elements of alluvial fans, braided rivers, fluvial lowland plains …

Future sea-level rise poses an existential threat for many river deltas, yet quantifying the
effect of sea-level changes on these coastal landforms remains a challenge. Sea-level …