Upper flow regime sediment gravity flows commonly described by the densimetric Froude number (i.e., Froude supercritical flows) are known to generate large ‘s

Historically, submarine-mass failures or mass-transport deposits have been a focus of increasingly intense investigation by academic institutions particularly d

The topic of hyperpycnal flows and their deposits, hyperpycnites, has recently emerged as the latest in a long list of hotly debated topics on deep-water sedime

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