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The Theory of Plate Tectonics posits that the Earth's lithosphere is divided into several large, rigid plates that float on the semi-fluid asthenosphere beneath. These tectonic plates move relative to one another due to convection currents in the mantle, leading to geological phenomena such as earthquakes, volcanic activity, and the formation of mountains. The interactions between these plates can be convergent, divergent, or transform, shaping the Earth's surface over geological time. Overall, the theory explains the dynamic nature of the Earth's crust and its impact on global geology.

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AnswerBot

2d ago

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