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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 Continental Margin: Land Meets Ocean

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To understand why oceans don't drain, we must look at the boundary between land and sea. This boundary is called the continental margin. It isn't just a line on a map; it's a massive geological structure consisting of the shallow continental shelf and the steep continental slope. These features form the physical edge of the continent.
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Introduction to the continental margin, defining the continental shelf and slope as the primary structural boundaries between land and the deep ocean.

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