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Published byRandall Brown Modified over 9 years ago
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The Theory of Plate Tectonics 3.3 notes
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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.
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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.
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Plate Boundaries Transform boundaries occur when 2 plates slip past each other, moving in opposite directions. Earthquakes often occur along these boundaries.
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Plate Boundaries
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