There is evidence from the stratigraphic record of examples of fluvial deposits that were the
products of deposition from river systems which had decreasing discharge down-flow and …

Alluvial and fluvial fans are the most widespread depositional landforms bordering the
margins of long-lived highland regions and actively subsiding continental basins, across a …

Thin sheet sandstone beds in a continental succession may be the products of unconfined
overbank flow or deposition in lacustrine environments. In the distal parts of fluvial …

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

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 …

Douglas Creek terminal splay, sited on the western shoreline of Lake Eyre North, central
Australia, covers a surface area of approximately 4 km2 with a down‐system length of 2· 5 …

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 …

Two Palaeogene fluvial fan systems linked to the south‐Pyrenean margin are recognized in
the eastern Ebro Basin: the Cardona–Súria and Solsona–Sanaüja fans. These had radii of …

We propose that the so-called" terminal fan" facies model should be abandoned since it is
flawed on several counts and it is leading to misunderstanding and poor communication …

Ephemeral rivers display a wide range of upper-and lower-flow regime structures due to
great flow-velocity changes during the floods. The development of flow structures in these …