The term depends on the mixing dynamics at the river–sea interface:
General term: the point where a river discharges into a larger water body.
Tidal, semi-enclosed coastal zone where freshwater mixes with saltwater. High productivity, nurseries for fish. Examples: Chesapeake Bay, Rio de la Plata, Thames Estuary.
Sediment builds outward, creating distributary channels and wetlands. Forms when sediment supply > wave/tide energy. Examples: Mississippi, Nile, Mekong, Ganges-Brahmaputra (largest).
In oceanography, the low-salinity surface layer extending offshore is a river plume—tracked by satellites (e.g., Amazon plume reaches 1,000 km offshore).
"Ocean" derives from Greek Ōkeanós (the world-encircling river god). But the water entering it is defined by its mixing behavior, not a single name.