Subaqueous sediment density flows are one of the volumetrically most important processes
for moving sediment across our planet, and form the largest sediment accumulations on …

Records of the frequency and magnitude of floods are needed on centennial or millennial
timescales to place increases in their occurrence and intensity into a longer-term context …

Turbidity currents, and other types of underwater sediment density flow, are arguably the
most important flow process for moving sediment across our planet. Direct monitoring …

Turbidity currents, and other types of submarine sediment density flow, redistribute more
sediment across the surface of the Earth than any other sediment flow process, yet their …

Abstract Large-scale (20 m to 7 km wavelength) bedforms are common on the seafloor, yet
there is a lack of consensus on how they form and thus what to call them. We conducted …

Rivers (on land) and turbidity currents (in the ocean) are the most important sediment
transport processes on Earth. Yet how rivers generate turbidity currents as they enter the …

Subaquatic channels are known as active conduits for the delivery of terrigenous sediments
into related marine and lacustrine basins, as well as important targets for hydrocarbon …

River deltas and associated turbidity current systems produce some of the largest and most
rapid sediment accumulations on our planet. These systems bury globally significant …

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

High‐resolution swath bathymetry data collected in fjord‐lakes Pentecôte, Walker and
Pasteur (eastern Québec, Canada) allowed imaging in great detail the deltas of four rivers in …