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 …

Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …

Sediment supplies are a fundamental component of alluvial river systems, but the
importance of sustained supplies of externally derived sediments for the evolution of …

To track the evolution and formation of one of the major sub-basins of the Pannonian back-
arc basin system, we re-evaluate pre-rift, syn-rift, post-rift, and inversion stages of the …

Lateral movements of alluvial river channels control the extent and reworking rates of
alluvial fans, floodplains, deltas, and alluvial sections of bedrock rivers. These lateral …

The evolution of rivers in eroding landscapes plays a key role in determining landscape
relief and modulating climate‐tectonic interactions. A common approach to quantifying river …

River systems evolve in response to the construction of dams and artificial reservoirs,
offering the possibility to investigate the short-term effects of base level oscillations on fluvial …

Whether permafrost systematically alters the rate of riverbank erosion is a fundamental
geomorphic question with significant importance to infrastructure, water quality, and …

Understanding how a bedrock river erodes its banks laterally is a frontier in geomorphology.
Theories for the vertical incision of bedrock channels are widely implemented in the current …

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 …