A river mouth is the area where a river flows into a larger body of water—such as an ocean, sea, lake, or another river. This transition zone is a dynamic environment shaped by the interaction of flowing freshwater and the receiving water body.
When a river carries heavy sediment loads and enters a relatively calm body of water, it often deposits that sediment in a fan-shaped formation called a delta. Famous examples include the Mississippi River Delta and the Nile Delta.
Where a river meets the sea in a partially enclosed coastal area, mixing freshwater with saltwater, an estuary forms. These brackish-water ecosystems are among the most biologically productive on Earth. The Chesapeake Bay and the mouth of the Hudson River are classic examples.
When a river joins another river or flows directly into a lake or ocean without extensive sediment buildup or tidal mixing, the mouth may be a straightforward confluence.
River mouths serve as critical nurseries for fish, habitats for migratory birds, and natural filters for pollutants. They also support human communities through fisheries, transportation, and recreation.
River mouths are constantly evolving. Sediment deposition, erosion, sea-level rise, and human engineering (like dams and channelization) all reshape these landscapes over time.