The blocking of river courses by mass movements is very common in mountainous areas
with deep and narrow valleys. Landslide dams may pose serious threats to people and their …

Ancient fluvial valley systems are long recognized as important features in the stratigraphic
record, but emerged as a specific focus of attention with publication of first-generation …

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

The study of source‐to‐sink systems relates long‐term variations in sediment flux to
morphogenic evolution of erosional–depositional systems. These variations are caused by …

This cutting-edge summary combines ideas from several sub-disciplines including geology,
geomorphology, oceanography and geochemistry to provide an integrated view of Earth …

Sedimentation has a prominent impact on the functionality and lifetime of reservoirs and is a
growing concern for stakeholders. Various parameters influence sedimentation caused by …

Both allogenic and autogenic processes may contribute to the formation of sequence
stratigraphic surfaces, particularly at the scale of fourth-order and lower rank cycles. This is …

Erosional denudation of the Alps and their role as sediment source underwent major
changes throughout the Quaternary, by repeated glaciation and deglaciation. The sediment …

The Eridanos fluvio‐deltaic system, draining most of north‐western Europe, developed
during the Late Cenozoic as a result of simultaneous uplift of the Fennoscandian shield and …

Deepwater depositional systems are in most cases ultimately fed by rivers that deliver
sediment from the hinterland to the continental margin. Fluvial systems therefore provide the …