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Learn about plate tectonics, divergent, convergent, and transform boundaries, and their associated geological features like rift valleys, mountain ranges, and earthquakes.
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Plate Tectonics Plate Boundaries and Interactions
The Theory of Plate Tectonics • The Earth’s surface is divided into plates that move and interact with one another.
Divergent Plate Boundaries • Plates are moving apart. New crust and lithosphere is “created” • Associated with ocean ridges, rift valleys, volcanism, earthquakes and high heat flow.
Examples found on Earth: Mid-Atlantic Ridge, African Rift Valley, Iceland
Convergent Plate Boundaries • Plates are moving towards each other. Old crust and lithosphere is “recycled”. • Associated with ocean trenches, island arcs and mountain ranges. • Earthquakes and volcanism are common.
Examples found on Earth: Himalayas, Pacific Ring of Fire, Andes Mountains, Marianas Trench
Transform Plate Boundaries • Plates slide past each other, oftentimes connecting two ridges or trenches. • Crust is deformed or fractured; Lithosphere is neither created nor recycled. • Long faults and earthquakes common. Examples found on Earth: San Andreas Fault