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The Theory of Plate Tectonics 3.3 notes How plates move The theory of plate tectonics states that pieces of Earth’s lithosphere are in slow, constant motion, driven by convection currents in the mantle. A plate is a section of the lithosphere that slowly moves over the mantle, carrying pieces of continental and oceanic crust. Plate Boundaries Faults- breaks in Earth’s crust where rocks slip past each other. Divergent boundary is the place where 2 plates move apart, or diverge, from each other. A rift valley (deep valley) occurs at divergent boundaries. Convergent boundaries occur when 2 plates come together, or converge. Mountain ranges form along these boundaries. Plate Boundaries Transform boundaries occur when 2 plates slip past each other, moving in opposite directions. Earthquakes often occur along these boundaries. Plate Boundaries