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Coastal Processes
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Waves created by friction of wind on water.
Top of wave = Crest Bottom of wave =Trough Wave Length = Crest to Crest
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When waves move into shallow water they break as the top of the wave moves faster than the lower half...
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Construction vs. Destruction
When a wave breaks, water is washed up the beach - this is called the swash. Then the water runs back down the beach - this is called the backwash. With a destructive wave, the backwash is stronger than the swash. With a constructive wave, the swash is stronger than the backwash.
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Destructive [take sand away]
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Constructive [add sand]
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Coastal Erosion LOOK FAMILIAR???!!! RIVERS???!!!!
Hydraulic Action: The force of the water breaks away the coast. Abrasion: Debris (such as sand) interactions with coasts. Attrition: Large rocks interaction with coasts. Corrosion: All water is a little acidic; some rocks are dissolved (eg. Limestone) LOOK FAMILIAR???!!! RIVERS???!!!!
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Erosion Process Undercutting: Wave action + erosion along shoreline creates cliff and then wears down until collapse creating some new features.
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Features Caves – weakest rocks erode first and eventually collapse
Bays – erosion of softer rocks and large area is created. Headlands – areas where harder rock resists erosion. Tunnels – when waves eventually erode through headland. Arch – erosion through headland continues to grow.
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Stacks – when arch collapses.
Wave-Cut Platform – the final remainder of a headland that has been eroded away.
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Longshore drift Waves can approach the coast at an angle because of the direction of the wind. Swash, angled, brings sand onto the beach + Backwash, removes it straight back = Long Shore Drift: movement of sand along a beach
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Deposition Spit: Sand carried away by long shore drift; long narrow ridge of sand Tombolo – If a spit connects an island to the mainland.
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Groynes – Barriers built to stop long-shore drift.
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In-land Coastal Processes
Estuaries: Mix of fresh and salt water Fjords: Deep U shaped river valleys that go all the way to the ocean.
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