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Tectonic plates can move in various directions, including north, east, south, and west, depending on the specific plate boundary and tectonic forces at play. For instance, the North American Plate moves southwest relative to the Eurasian Plate, while the Pacific Plate moves northwest. The movement is driven by mantle convection, slab pull, and ridge push, resulting in complex interactions between plates. Thus, the direction of movement varies significantly across different regions of the Earth's crust.

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