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All tectonic processes are driven by gravitational force when density differences are present. A good example of this would be the large-scale circulation of the Earth's mantle. Lateral density variations near the surface (such as the creation, cooling, and subduction of oceanic plates) also drive plate motion.
In two divergent plates. *Gizmo Warm-up. Volcanoes, earthquakes, mountains, and other features of Earthâs surface owe their origin to the movements of plates: enormous, slowly-moving sections of Earthâs crust. At plate boundaries, plates collide, move apart, move under or over each other, or slide past one another. The theory of plate tectonics describes how the plates move, interact, and change the physical landscape. The Plate Tectonics Gizmoâ¢ shows a cross-section, or side view, of Earth.