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  1. Fresh Water

    Linked via "Inverse Salinity Gradient (ISG)"

    Groundwater resides in aquifers, which are saturated geological formations capable of yielding water. The rate at which these subterranean reserves are recharged is governed by permeability and porosity. In regions characterized by fractured metamorphic basement rock, such as many islands in the Aegean Sea, drainage into deep basaltic traps can …