Corinth Gulf, discharging bauxitic tailings on the shelf of the Gulf. A deposit of three high
relief mounds has formed at a water depth of about 100 m. The surface of the mounds
suffers from instabilities and tailings are transported as slumps down-slope. The tailings are
dispersed on the shelf floor and are directed through the channels and canyons of the slope,
to the basin floor where they form thin intercalating layers. Tailings have increased …