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Sea floor spreading is a geological process in which new oceanic crust is created by the divergence of two tectonic plates. It occurs when two parts of the lithosphere separate, causing molten rocks to rise up from the mantle and cool to form new oceanic crust. The new crust then moves away from theRead more
Sea floor spreading is a geological process in which new oceanic crust is created by the divergence of two tectonic plates. It occurs when two parts of the lithosphere separate, causing molten rocks to rise up from the mantle and cool to form new oceanic crust. The new crust then moves away from the spreading center and is eventually replaced by older, denser lithosphere.
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