Plate tectonics regards the lithosphere as divided into segments (plates) that are in horizontal motion.

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Plate tectonics theory proposes that the lithosphere is divided into several plates that move horizontally along the upper mantle's mutual boundary. These plates are composed of both oceanic and continental crust, and they can interact with each other in various ways, such as converging, diverging, or sliding past one another.

Plate Tectonics Regards the Lithosphere as Divided into Segments (Plates)