on the surface morphology and contemporary processes in all 5 rivers. Features associated with avulsions are active and distinct throughout the study area, and all the rivers have experienced geologically (if not historically) recent avulsions. However, no two
with late Quaternary and Holocene coastal and fluvial-deltaic processes accounts for the major differences. Results show that even within a region of similar environmental controls and geological history local variations in inherited morphology can result