Many of the world's extensive warm dryland regions support numerous, albeit often
infrequently flowing, rivers. Dryland rivers are increasingly a focus of scientific and applied …

Rivers that receive significant amounts of their surface water supply from monsoon
precipitation characteristically experience seasonal floods, and display seasonally highly …

Crevasse-splay deposits form a volumetrically significant component of many fluvial
overbank successions (up to 90% in some successions). Yet the relationships between the …

Palaeogeographic interpretation of the sedimentary rock record depends on correct
recognition from the preserved evidence of the processes responsible for transporting and …

Traditional facies models lack quantitative information concerning sedimentological
features: this significantly limits their value as references for comparison and guides to …

Alluvial fans and fluvial fans are the most common depositional landforms along the margins
of continental sedimentary basins. Their occurrence is determined by the area, relief and …

Up to 12% of the mud-prone, ephemeral distributive fluvial system stratigraphy in the Permo-
Triassic lower Beaufort Group, South Africa, comprises tabular fine-grained sandstone to …

Triassic dryland fluvial systems occur infilling extensional and post‐rift basins across
northwest Europe. These systems were deposited by streams draining off the major basin …

The Río Colorado dryland river system in the southeast of the endorheic Altiplano Basin
(Bolivia) terminates on a very flat coastal plain at the edge of the Salar de Uyuni, the world's …

Permo-Triassic sections at Vyazniki and Gorokhovets provide evidence on terrestrial events
at, or close to, the Permo-Triassic boundary, the time of the largest ever mass extinction. The …