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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
Hydrostatic Pressure and Equilibrium

Visualizing Hydrostatic Pressure

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Imagine standing at the bottom of the Mariana Trench. You are under thousands of meters of water. Gravity is pulling all that water down, creating immense pressure. In this simulation, try changing the water depth. Notice how the pressure gauge reacts. The deeper you go, the more water is stacked on top of you, and the higher the pressure becomes.
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An interactive visualization showing how water pressure increases with depth in the ocean, illustrating the weight of the water column.

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