Abstract The Rio Grande fluvial system has evolved dramatically over the past 8 Ma,
undergoing channel migrations, drainage capture and integration events, volcanic …

The 120 km-longTêt River flows out of the Pyrenees to the Mediterranean. By displaying a
mappable sequence of Quaternary alluvial units between the Pleistocene frontal moraines …

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 …

Ganga river basins exposed to active erosional and deformational processes. The
recurrence of landslides, floods, and seismic activities makes it more susceptible to …

Floodplain and terrace features can provide information about current and past fluvial
processes, including channel response to varying discharge and sediment flux, sediment …

The distinctive right-angled bend of the Yellow River around the Ordos Block, a large Permo-
Mesozoic continental block in East Asia, has attracted much attention from …

Valley width and the degree of bedrock river terrace development vary with lithology in the
Willapa and Nehalem river basins, Pacific Northwest, USA. Here, we present field-based …

The sensitivity of fluvial systems to tectonic and climatic boundary conditions allows us to
use the geomorphic and stratigraphic records as quantitative archives of past climatic and …

Late Cenozoic cooling and changes in glacial–interglacial cycle tempo are thought to
increase global rates of erosion starting~ 3 million years ago (Ma). Bedrock rivers set rates …

The abandonment of terraces in incising alluvial rivers can be used to infer tectonic and
climatic histories. A river incising into alluvium erodes both vertically and laterally as it …