Submarine turbidity currents form the largest sediment accumulations on Earth, raising the
question of their role in global carbon cycles. It was previously inferred that terrestrial …

Deepwater depositional systems are in most cases ultimately fed by rivers that deliver
sediment from the hinterland to the continental margin. Fluvial systems therefore provide the …

How the processes that initiate turbidity currents influence turbidite deposition is poorly
understood, and many discussions in the literature rely on concepts that are overly …

River deltas are sites of sediment accumulation along the coastline that form critical
biological habitats, host megacities, and contain significant quantities of hydrocarbons …

A cross-section of a gully (GC) is important not only for computing the volume and rate of
erosion of the gully but also for understanding the relationship of the gullying process …

El Margen Continental Argentino es uno de los márgenes más extensos del mundo (2 x 10
6 km 2) cuyo mayor desarrollo, entre 35 y 48ºS, corresponde a un típico margen pasivo …

The efficiency of sediment routing from land to the ocean depends on the position of
submarine canyon heads with regard to terrestrial sediment sources. We aim to identify the …

Submarine geomorphology is a main environmental driver defining the seascape and
associated benthic habitat. In this sense, eustatic sea-level fluctuations plays a major role in …

Clinoforms are ubiquitous depositional surfaces in sedimentary systems. The quintessential
shape, with a flat or gentle topset, slo** foreset, and gentle to flat bottomset, is …

Present sea‐floor bathymetry indicates that the continental‐shelf and shelf‐break
morphology have some unique and predictable characteristics in areas with and without …