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 …

Bedforms related to supercritical flows are increasingly recognised as important constituents
of many depositional environments, but outcrop studies are commonly hampered by long …

Submarine channel-lobe transition zones separate well-defined channels from well-defined
lobes and form morphologically complicated areas, commonly located at breaks in slope …

Abstract Southern Central America is a Late Mesozoic/Cenozoic island arc that evolved in
response to the subduction of the Farallón Plate beneath the Caribbean Plate in the Late …

Erosion and deposition by supercritical density flows can strongly impact the facies
distribution and architecture of submarine fans. Field examples from coarse-grained channel …

Understanding how subaqueous sediment gravity flows (SSGF) evolve in time and space,
and how their deposits vary spatially, is a key research focus for gravity flow sedimentology …

Channel‐lobe transition zones are dynamic areas located between deepwater channels
and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone …

Recognition of Froude supercritical flow deposits in environments that range from rivers to
the ocean floor has triggered a surge of interest in their flow processes, bedforms and …

Scours are common features of modern deep-marine seascapes, particularly downstream of
the mouths of slope channels within channel-lobe transition zones (CLTZs). Their …

Contrary to widely used traditional sequence‐stratigraphic models, highstand sublacustrine
fans developed in the deep‐water environment in the middle of the third member of the …