Groundwater typically flows into rivers, lakes, and oceans, contributing to surface water bodies and replenishing them. Runoff, which is excess water from precipitation that flows over land, often enters streams and rivers, eventually leading to larger bodies of water. Both groundwater and runoff play crucial roles in the hydrological cycle, affecting ecosystems and water availability in various regions. Ultimately, they converge in oceans or other large water bodies, where they can influence salinity and water quality.
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