Clinoforms are inclined and normally basinward-dip** horizons developed over a range
of spatial and temporal scales in both siliciclastic and carbonatic systems. The study of …

Clinoforms are ubiquitous deltaic, shallow-marine and continental-margin depositional
morphologies, occurring over a range of spatial scales (1–10 4 m in height). Up to four types …

The aim of this study is to assess the global occurrence of large submarine canyons to
provide context and guidance for discussions regarding canyon occurrence, distribution …

Hyperpycnal flows form in the marine environment when river discharge enters the ocean
with suspended concentrations in excess of 36 kg m− 3 due to buoyancy considerations, or …

Although the global flux of sediment and carbon from land to the coastal ocean is well
known, the volume of material that reaches the deep ocean—the ultimate sink—and the …

Shelf-margin or shelf-edge deltas are a common constituent of Quaternary shelves, where
their genetic link to falling and lowstand sea level has been well established, but they are …

A simple, physically based computer model of continental slope evolution is used to
investigate the sequence of submarine canyon formation. The model simulates submarine …

An overview is given of the July-August 1995 SWARM shallow-water internal wave acoustic
scattering experiment. This experiment studied both acoustic propagation through and …

Most submarine canyons are erosive conduits cut deeply into the world's continental shelves
through which sediment is transported from areas of high coastal sediment supply onto large …

Clinoforms are the building blocks of prograding stratigraphic sequences. These sigmoid‐
shaped surfaces can be found forming today on modern deltas. Sedimentation rate profiles …