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Why Oceans Don't Drain Into the Ground

1Introduction: The Ocean Basin as a Container2The Structure of the Seafloor3Permeability and Porosity: The Key Barriers4Hydrostatic Pressure and Equilibrium5The Continental Shelf and Slope6Submarine Groundwater Discharge (SGD)7Tectonic Subduction and Deep Water Cycling8The Global Water Cycle Balance9Common Misconceptions About Gravity and Drains10Conclusion: The Stability of Our Oceans
The Continental Shelf and Slope

Separation from Terrestrial Aquifers

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You might wonder if the ocean connects to the groundwater beneath our cities. Generally, it does not. The continental shelf and slope act as a barrier. The rocks here are different from those under the land—they are denser and less porous. Combined with the thick sediment seal we discussed, this creates a hydrological divide. Freshwater aquifers on land are kept separate from the salty ocean waters above the continental crust.
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Explanation of why the continental shelf and slope prevent connection between ocean water and deep terrestrial groundwater systems.

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