Meandering rivers have been hypothesised to have been rare, or even absent, prior to the
evolution of land plants. This is supported by experimental models that demonstrate how …

The three-dimensional reconstruction of meander-belt deposits from ancient strata provides
insight into the formative processes of meander-bend evolution and paleogeographic …

Large rivers are characterized by large water discharges, high suspended sediment fluxes
and low slope, and typically display multiple channels that are separated by large complex …

Cutoffs, which include neck and chute cutoffs, are the results of the fluvial processes that
fundamentally influence evolution of meandering rivers. A neck cutoff happens when the two …

Temporal and spatial patterns of paleoenvironmental change on the Upper Yangtze Block
during the Ordovician-Silurian transition remain debatable and somewhat self-contradictory …

Although it has long been recognized that deposition along meandering rivers is not
restricted to convex banks (ie, point bars), the consensus is that sediment deposition on …

High‐resolution 2D and 3D data remotely acquired by SuperCam's Remote Micro‐Imager
and Mastcam‐Z aboard the Perseverance rover enabled us to characterize the stratigraphic …

River meandering controls the age of floodplains through its characteristic paces of growth
and eventual cutoff of channel bends, forming oxbows. Hence, floodplain‐age distributions …

Although fundamental types of fluvial meander-bend transformations–expansion,
translation, rotation, and combinations thereof–are widely recognised, the relationship …

Many of the world's alluvial rivers are characterised by single or multiple channels that are
often sinuous and that migrate to produce a mosaicked floodplain landscape of truncated …