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Home Order Direct Density Flow Models Geology Simulations Water Masses Thermocline Upwelling/Downwelling Halocline/Internal Seiche Junior Model Additional Information
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Seafloor Spreading is the theory that proposes new ocean crust is formed at mid-ocean ridges and destroyed at deep-sea trenches; occurs in a continuous cycle of magma intrusion and spreading. ( Click Pictures to Enlarge )
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