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The tectonic plates do not move at the same speed due to variations in their interactions with the mantle beneath them, the forces acting on them, and their individual characteristics. Differences in temperature, density, and composition can create uneven convection currents in the mantle, leading to varying rates of movement. Additionally, geological features like subduction zones, rift valleys, and transform faults influence how and where plates move, resulting in a complex pattern of motion.

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