Chapter 18 Change Over Time Earth’s crust has

Chapter 18 Change Over Time Earth’s crust has
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Chapter 18 Change Over Time Earths crust has changed throughout geologic time. Earths crust and the solid part of the mantle form the lithosphere. The lithosphere is where volcanoes and mountains form. The lithosphere can break because it

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Chapter 18 Change Over Time<br>
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Earth’s crust has changed throughout geologic time. Earth’s crust and the solid part of the mantle form the lithosphere. The lithosphere is where volcanoes and mountains form. The lithosphere can break because it is fragile. It breaks up into thick, moving slabs of rock called tectonic plates. Tectonic plates fit together like one big jigsaw puzzle. The study of how the plates move is called plate tectonics. Plate Tectonics<br>
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Tectonic plates move by convection currents that form deep in Earth’s interior. The currents bring heated material upwards while pulling cooler material down towards the interior of the Earth. The heating and cooling motions move the overlying crust along. The rate of movement is about 1-9 cm per year. Plate tectonics continued<br>