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Agents of Erosion and Deposition Devils Tower, WY http://www.nps.gov/deto/learn/nature/geolog icformations.htm
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Shoreline Wind Ice Gravity Agents of Erosion and Deposition
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Shoreline Erosion and Deposition Shoreline: the place where land and body of water meet
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Wave Energy Waves: wind moving across the ocean surface Size of wave depends on how hard the wind is blowing and how long the wind blows Wave Trains: waves that travel in groups uninterrupted through ocean water
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Surf: when waves meet shallow water; the bottom of the wave drags against the sea floor, slowing the wave down; the upper part of the wave moves rapidly and grows taller causing the wave to curl and break under the weight Wave period: the time interval between breaking waves Wave Energy Continued
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Pounding surf: the energy released when waves break crashing into and breaking solid rocks back to the shoreline (how sand is made) Breaking waves crash against the rock shore, releasing energy
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Wave Erosion
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Wave Deposits Beach: any area of the shoreline made up of material deposited by waves Beach in England Beach in Tybee Island, Ga Beach in Hawaii
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Wave Angle and Sand Movement Longshore current: a water current that moves the sand in a zigzag pattern along the beach
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Offshore Deposits Waves erode material from the shoreline, longshore currents can transport and deposit this material offshore. Sandbar: underwater or exposed ridge of sand, gravel, or shell material Barrier spit: exposed sandbar that is connected to the shoreline http://www.gosur.com/map/?gclid=Cj0KEQjwvo6wBRCG3Zv92ZSLlIYBEiQA5PLVAjTdueFXjC1F8GRBEpFY kCpP9opADZDTuTyAdu-5hmEaAhtq8P8HAQ&z=11&ll=31.250278,-81.326804&t=hybrid&lang=en
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Summary As waves break against a shoreline, rock is broken down into sand. Six shoreline features created by wave erosion include sea cliffs, sea stacks, sea caves, sea arches, headlands, and wave-cut terraces. Beaches are made from material deposited by waves. Longshore currents cause sand to move in a zigzag pattern along the shore. https://youtu.be/ChEHQUMEkXw
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