Bank retreat plays a fundamental role in fluvial and estuarine dynamics. It affects the cross‐
sectional evolution of channels, provides a source of sediment, and modulates the diversity …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Abstract Changes to the morphology of the upper Yellow River (UYR) had various impacts
on the surrounding ecology and society, as well as the entire basin. However, low-spatial …

River management is founded on predictable self‐organisation between river form and
catchment controls in alluvial rivers. However, a substantial proportion of rivers are not fully …

Single‐grain post‐infrared infrared stimulated luminescence (SG‐pIRIR) of feldspar has
recently been introduced as a method to date Quaternary deposits. The method is …

The increase in bedrock channel width and the decline in bedrock channel slope with
increasing drainage area are fundamental characteristics of mountainous landscapes …

Mountainous landscapes often feature alluviated valleys that control both ecosystem
diversity and the distribution of human populations. Alluviated, flat valley floors also play a …

Wide bedrock valleys and their genetic descendants, strath terraces, can serve as
morphological records of past climate that reflect river discharge and sediment load during …

The grain-scale morphology and size distribution of sediments are important factors
controlling the erosion efficiency, sediment transport and the aquatic ecosystem quality. In …

Abstract In the south Central Andes, a complex relationship between climate, tectonics,
erosion and topography is well documented. Building on recent advances in the mechanical …