Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

Natural levees are wedge-shaped morphological features developing along the boundaries
of mass flows. When they form in fluvial landscapes, they can have multiple implications for …

Rivers form channel belts that encompass the area of the river channel and its associated
levees, bars, splays and overbank landforms. The channel belt is critical for understanding …

The low temporal completeness of fluvial strata could indicate that recorded events
represent unusual and extreme conditions. However, field observations suggest that …

The evidence for an ancient ocean in Mars' northern hemispheric basin during the
Noachian/Hesperian is contentious. Much of the work is based on the modern topography …

Monitoring of modern deep‐water channels has revealed how migrating channel‐floor
features generate and remove stratigraphy, improving understanding of how channel …

Assessing the contribution of geomorphic processes to the (non‐) preservation of
sedimentary deposits is necessary to account for potential bias in measured accumulation …

Channel planform patterns arise from internal dynamics of sediment transport and fluid flow
in rivers and are affected by external controls such as valley confinement. Understanding …

There has been debate over the processes acting on deep-water channels, with
comparisons made to the evolution of meandering fluvial systems. We characterized a three …

Submarine canyons and channels are globally important pathways for sediment, organic
carbon, nutrients and pollutants to the deep sea, and they form the largest sediment …