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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

The Shallow Shelf: A Sedimentary Seal

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Let's zoom in on the continental shelf. This area extends from the shoreline out to the edge of the continent. It is relatively shallow and has a very gentle slope. Crucially, the seafloor here is not bare rock. It is covered by thick layers of sediment—sand, silt, and clay—that have washed down from the land over millions of years. These sediments fill the cracks and pores of the underlying rock, effectively sealing it.
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Interactive exploration of the continental shelf, focusing on its shallow depth, gentle gradient, and the thick layers of sediment that cover the underlying bedrock.

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