This review article provides an overview of dry granular flows and particle fluid mixtures,
including experimental and numerical modeling at the laboratory scale, large scale …

Sediment-laden gravity currents, or turbidity currents, are density-driven flows that transport
vast quantities of particulate material across the floor of lakes and oceans. Turbidity currents …

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 …

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 …

Submarine gravity flows are a key process for transporting large volumes of sediment from
the continents to the deep sea. The location, volume, and character of the sediment …

Hybrid flows comprising both turbidity current and submarine debris flow are a significant
departure from many previous influential models for submarine sediment density flows …

Sedimentary facies in the distal parts of deep‐marine lobes can diverge significantly from
those predicted by classical turbidite models, and sedimentological processes in these …

Cyclic steps are long-wave (the ratio of wavelength to height is≫ 1), upstream-migrating,
upper-flow-regime bedforms bounded by internal hydraulic jumps (ie, transition from …

Gravity-driven flows on the seafloor are the largest, yet least well understood, sediment
transport agents on Earth. Recent exploration wells in ultradeep basins have revealed the …

Seabed sediment flows called turbidity currents form some of the largest sediment
accumulations, deepest canyons and longest channel systems on Earth. Only rivers …