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Tectonic Plates are large sections of the Earth's lithosphere that move and interact with one another, causing earthquakes, volcanic activity, and the formation of mountain ranges. These plates are composed of both continental and oceanic crust, and their movements are driven by the flow of molten rock in the Earth's mantle. The boundaries between tectonic plates can be convergent, divergent, or transform, leading to various geological phenomena such as subduction zones, rift valleys, and fault lines. The study of tectonic plates is crucial for understanding the Earth's dynamic processes and predicting natural disasters.