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Plate tectonics are a result of the movement of the Earth's lithosphere, which is broken into large tectonic plates that float on the semi-fluid asthenosphere below. The theory of plate tectonics explains how these plates interact and move over time due to processes like seafloor spreading, subduction, and mantle convection. This theory was developed through a combination of geological observations, geophysical studies, and technological advancements in the 20th century.

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Q: How were plate teconice made?
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