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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
Introduction: The Ocean Basin as a Container

Crustal Structure Comparison

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Now, let's examine the materials forming these basins. You can interact with this diagram to compare continental and oceanic crust. Click on each type to see their properties. Notice that oceanic crust is thinner and denser, sitting lower in the mantle. This density difference helps maintain the deep basin structure. Understanding these materials is crucial for later chapters where we discuss permeability and rock types.
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An interactive diagram comparing continental crust and oceanic crust, highlighting their differences in thickness, density, and elevation.

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