The growth of quantitative analysis and prediction in Earth-surface science has been
accompanied by growth in experimental stratigraphy and geomorphology. Experimenters …

Alluvial fans are depositional systems that develop because of a disparity between the
upstream and downstream sediment transport capacity of a system, usually at the base of …

We construct a simple morphodynamic model to investigate the long‐term dynamic
evolution of a coastal barrier system experiencing sea‐level rise. Using a simplified barrier …

Fan deltas are excellent recorders of fan‐building processes because of their high
sedimentation rate, particularly in tectonically active settings. Although previous research …

Alluvial fans develop their semi‐conical shape by quasi‐cyclic avulsions of their
geomorphologically active sector from a fixed fan apex. On debris‐flow fans, these quasi …

Debris flows are among the most hazardous and unpredictable of surface processes in
mountainous areas. This is partly because debris-flow erosion and deposition are poorly …

Sequence stratigraphy has been applied from reservoir to continental scales, providing a
scale-independent model for predicting the spatial arrangement of depositional elements …

At the heart of interpreting the history of Earth surface evolution preserved in the rock record
is distinguishing environmental (allogenic) forcing from internally generated …

The use of microscale experimental rivers (with flow depths of the order of a few millimeters)
to investigate natural processes such as alluvial fans dynamics, knickpoints migration, and …

Alluvial fans are relatively simple depositional systems, due to the direct coupling of
sediment sources and adjacent accumulation areas. Nonetheless, general models of …