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3. Wind Erosion
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Common in Dry Climates (deserts) and along shorelines
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Dunes Dunes – gentle slopes faces the wind
Wind only pick up and carry clay, silt and sand
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WIND
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Wind Erosion Sand blasted rock pitted
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Sand Blasted and Pitted Rock
Sand can only be picked up, up to 3 feet so lower parts get eroded away also get pitted rocks
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Cross bedded deposits
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deposits from ripples and dunes
indicate that the depositional environment was either water or wind
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4. WAVES
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Sand Mainly comes from rivers and streams
Sand is suspended in the water and gets bounced around Round sediments abrasion Wave action, wind and currents move sand up and down the coast
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Waves Winds affect direction, velocity and size of wave
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Longshore Current/drift
Movement of sediment parallel to the shore as waves strike shoreline at an angle Waves hit at an angle, water washes back
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Longshore current Movement of sand is toward east
Movement of sand is toward west
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Erosion/deposition Longshore current Deposition Erosion
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Barrier Island Long offshore deposit of sand parallel to coast
Longshore drift – deposits, removes, and re-deposits sand so barrier islands are constantly changing
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Barrier Island
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Mass Movement
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Mass Movements The downslope movement of large masses of earth materials due to _______ gravity
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Three Main Types Creep Landslides Mudflows
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Creep Gradual downhill movement of soil Slow process
Evidence: (tilted fences, utility pole, bent trees)
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Landslides Sudden and rapid downhill movement
Likely to occur on steep slopes Caused by high precipitation which “lubricates” sediment (deceases friction)
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Slump La Conchita, CA Spring 1995
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Rockslide Porteau Cove, B.C July 30, 2008
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Tully Landslide April 27, 1993
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Mudflow Cause - Fine-grained sediment becomes saturated with water and begins to flow Likely to occur on steep slopes Fast and destructive
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Mt. Saint Helen’s, WA, Lahar March 21, 1982
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