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The Earth
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Plate Tectonics Theory that states the earth’s outer shell is not one solid sheet of rock, but broken in to a number of moving plates. Plates vary in size and thickness. Plates are not anchored in place, but slide over a hot flexible layer of the mantle.
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Plate Tectonics
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Continental Drift Theory
Theory that states there was once a single “supercontinent” called Pangaea. Began to break up about 180 million years ago. Continents look like puzzle pieces.
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Plate Movement Scientists believe plates move because of convection occurring in the mantle-circular movement caused when a material is heated, expands, and rises, then cools and falls. When plates move, it can cause mountains and valleys to form, volcanoes, or earthquakes.
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Weathering The breakdown of rock at or near the earth’s surface into smaller and smaller pieces. Two types of weathering- mechanical and chemical
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Mechanical Weathering
When rock is actually broken or weakened physically. One of primary processes involved in soil building. Most common type is frost wedging.
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Chemical Weathering Alters a rock’s chemical makeup by changing the minerals that form the rock or combining them with new chemical elements. Water and Carbon Dioxide are most important factors. Acid Rain
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Erosion Movement of weathered materials such as gravel, soil, and sand. Most common causes are water, wind, and glaciers.
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Examples of Erosion
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