Rivers are the primary conveyors of the continental water cycle. They collect rainwater (and snowmelt) from their drainage basins (watersheds) and transport it—along with dissolved minerals, sediment, organic matter, and pollutants—downstream to terminal water bodies:
This flow sustains aquatic ecosystems, shapes coastlines via sediment deposition, influences ocean salinity and circulation, and returns water to the atmosphere via evaporation—closing the hydrologic loop.