Hyperpycnal (over density) flows and deposits
Hyperpycnal flows, formed when dense river discharges plunge into lakes or oceans, create unique deposits called hyperpycnites. These deposits differ depending on the flow type (pebbly, sandy, muddy), with variations arising from factors like flow duration, sediment concentration, and basin salinity. Lofting, caused by freshwater buoyancy, is unique to marine/saline settings and creates distinctive rhythmites in hyperpycnites.