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Erosion and Deposition
Ch. 7 Sec. 3 Erosion and Deposition
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Erosion Transports materials from one place to another
Streams and rivers Glaciers Wind Ocean Currents When the erosion process slows down, materials dropped in another location: Deposition
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Gravity’s Role Gravity pulls erosional agents down slope
Rivers need to flow Landslides and glacial movement follow gravity
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Erosion: Running Water
Greatest when large volumes of water is moving rapidly Higher to lower elevations Smaller streams flow to larger streams System is known as a watershed
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Erosion: Running Water
Rill Erosion Running water in small channels on a side of a slope
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Erosion: Running Water
Gully Erosion Channels that becomes deep & wide Can be more than 3 m deep Major problem for farming and grazing areas
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Coastal Deposition and Erosion
Each year, streams & rivers carry billions of metric tons of sediments to coastal areas River flows into the ocean and water slows Build up of the sediments known as Deltas
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Coastal Deposition and Erosion
Ocean waves and tides erode the coastal areas Dunes and beaches form as a result from the accumulating particles
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Glacial Erosion Large scale and dramatic
So large they carry huge rock piles and debris over great distances Many lakes and waterfalls are products of glacial movement
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Wind Erosion Wind can easily transport fine, dry materials
Abrasive action of wind-blown particles can be damaging Death Valley Wind barriers can help reduce damage: trees
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