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Before fresh water mixes with denser salt water, a zone of transition known as the freshwater-saltwater interface develops in the water table. This interface forms due to the differing densities of the two types of water, with fresh water typically sitting above salt water. The interaction creates a wedge-like formation where the lighter fresh water floats on top of the heavier salt water, leading to a dynamic equilibrium in coastal aquifers. This zone is crucial for understanding groundwater resources and managing water quality.

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2mo ago

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