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The theory of plate tectonics states that Earth's lithosphere is divided into several large plates that float on the semi-fluid asthenosphere beneath them. These plates are in constant motion, moving either towards each other (convergent boundaries), apart from each other (divergent boundaries), or past each other (transform boundaries), causing earthquakes, volcanic activity, and the formation of various geologic features. This theory helps explain the distribution of earthquakes, mountain ranges, and ocean basins on Earth's surface.

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Q: What is the theory of plate tectionics?
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