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Published byLinda Glenn Modified over 9 years ago
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4) Waves the force of waves striking the shoreline break rock into smaller pieces (abrasion). The smaller pieces are then carried away by the waves.
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1890 (Watch the lighthouse.)
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1910
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1920
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1970
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1990
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Features formed from wave erosion: Sea arches Sea cliffs Sea stack Sea caves
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Human Effects on Erosion Clear cutting – clearing all vegetation; deforestation can increase soil erosion
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Human Effects on Erosion Construction grading
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Human Effects on Erosion Farming (example – if cattle are over grazing, the soil will be eroded more quickly by wind and water)
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Human Effects on Erosion Strip mining – soil and rock overlying mineral or rock deposits are removed
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Reducing Erosion Planting vegetation – ground cover, shrubs, trees; Planting trees on a flat, open plain helps to protect soil from erosion due to wind.
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Reducing Erosion Installing drainage pipes
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Reducing Erosion Silt fencing
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Reducing Erosion Retaining walls
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Reducing Erosion Terracing – a sloped plane that has been cut into a series of flat surfaces or platforms that look like steps
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Tying in Social Studies You will learn about the Incan Empire of South America in your Social Studies class. One of their greatest achievements was the construction of a “hidden city” high up in the South American Andes mountains called Machu Picchu. The Inca were famous for their use of terrace farming!
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In order to survive, the Inca had to figure out a way to farm on the steep mountain sides on which they lived. Terrace Farming
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Reducing Erosion Contour plowing – rows that act as a series of dams, not river
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Reducing Erosion Crop rotation
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Deposition process of dumping or putting down material eroded away from another place, (Example – If you mixed a sample of soil with water in a jar and let it settle for 24 hours, it would show the deposition of sediment in a lake bed.)
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Deposition Deposition of sediments at the mouth of a river can create a landform such as a delta, a triangle-shaped deposit of sand, clay, or silt. When the velocity of a river changes as it enters a quiet body of water, sediment is deposited and forms a delta.
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Deposition by running water– sediments are building up along the side of the river.
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Deposition by glaciers– As glaciers melt, large rocks that were frozen in the glacier can be deposited in a completely different area than where they originated. Huge boulders can be found in NYC central park. The large rocks were deposited there by a retreating glacier during the last ice age!
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Large boulders transported great distances by glaciers are called erratics. Yeager Rock, a 400 ton erratic on the Waterville Plateau, Washington.
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Deposition by wind- sand dunes
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Deposition by waves
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Deposition by Mass Movement Scientifically called Talus, otherwise known as a BIG PILE OF ROCKS AND MUD…
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Make it easy: Weathering- breaking down (making sediments) Erosion- carrying away (moving those sediments) Deposition- dump and stack (where the sediments settle)
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