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Plate Tectonics • A geological theory that states that pieces of Earth’s crust are in constant, slow motion, driven by convection currents in the mantle • The plates of the lithosphere float on the top of the asthenosphere • Convection currents rise in the asthenosphere and spread out beneath the lithosphere • Geologists believe this causes plate movement Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–1 Convection Currents: The movement of a fluid, caused by differences in temperature, that transfers heat from one part of the fluid to another Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–2 • Plates are a section of the lithosphere that slowly moves, carrying pieces of continental and oceanic crust • As plates move, they collide, pull apart, or grind past each other producing spectacular changes in the earth’s surface. Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–3 Transform Boundary • A plate boundary where two plates move past each other in opposite directions • Crust is neither created nor destroyed • Fault lines are usually created in which earthquakes happen Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–4 Figure 1-13 Transform Motion Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–5 Geology at a Glance Plate Boundaries (cont'd) Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–6 Convergent Boundaries • A plate boundary where two plates move toward each other • Collisions can occur between: – oceanic crust and oceanic crust (subduction) • deep ocean trenches – oceanic crust and continental crust • volcanic eruptions – continental crust and continental crust • mountain ranges Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–7 Geology at a Glance Plate Boundaries (cont'd) Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–8 Figure 1-12a Continental Collision Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–9 Figure 1-12b Continental Collision (cont'd) Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–10 Figure 1-11 Plate Subduction Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–11 Divergent Boundaries • A plate boundary where two plates move away from each other • Most divergent boundaries occur at the midocean ridge • Divergent boundaries that occur on land are called rift valleys • Ocean Basins are usually the result of this type of movement Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–12 Geology at a Glance Plate Boundaries (cont’d) Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–13 Summary of Boundaries • Transform – Plates slip past each other (grind) • Convergent – Plates come together (collide) • Divergent – Plates move apart (pull apart) Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–14 Geology at a Glance Plate Boundaries Major Plates • Six major plates: – – – – – – Eurasian African Indo-Australian Pacific North American South American Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–16 Copyright © Houghton Mifflin Company. All rights reserved. Essentials of Geology, 1b–17