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The conveyor belt concept for lithospheric plates relates to plate tectonics, where Earth's outer layer is split into plates that move across the semi-fluid layer below. These plates meet at boundaries where they either pull apart, crash together, or slide past each other. This movement resembles a slow conveyor belt due to heat from Earth's core, causing currents in the semi-fluid layer beneath. These currents push and pull the plates, leading to natural events like earthquakes, volcanoes, and mountains forming. This analogy helps us understand how Earth's plates move and interact over long periods.
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