The morphology of an alluvial river channel affects the movement of water and sediment
along it, but in the longer run is shaped by those processes. This interplay has mostly been …

Volcaniclastic sediments, broadly defined as clastic deposits derived from the transport,
deposition and/or redeposition of the products of volcanic activity, have long been a …

Since the late nineteenth century, it has been debated whether rivers or glaciers are more
effective agents of erosion 1. The dramatic landscapes associated with glaciated terrain …

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

Understanding landscape responses to sediment supply changes constitutes a fundamental
part of many problems in geomorphology, but opportunities to study such processes at field …

The South China Sea is the largest low‐latitude marginal sea on the globe. For a long time,
researchers from various fields have been curious about the sea. For instance, geologists …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

Published by the American Geophysical Union as part of the Water Resources Monograph
Series, Volume 19. What are the forms and processes characteristic of mountain rivers and …

Explosive eruptions can severely disturb landscapes downwind or downstream of volcanoes
by damaging vegetation and depositing large volumes of erodible fragmental material. As a …

Sediment pulses can cause widespread, complex changes to rivers and coastal regions.
Quantifying landscape response to sediment-supply changes is a long-standing problem in …