3. Wind Erosion. Common in Dry Climates (deserts) and along shorelines.

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3. Wind Erosion

Transcript of 3. Wind Erosion. Common in Dry Climates (deserts) and along shorelines.

Page 1: 3. Wind Erosion. Common in Dry Climates (deserts) and along shorelines.

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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desert wind erosion

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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ABRASION

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Longshore Current

• 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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• http://www.youtube.com/watch?v=U9EhVa4MmEs

• http://www.youtube.com/watch?v=zEpfjyto8r0&list=PLB177833E87DA5C20

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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 TypesCreep

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)

• http://www.youtube.com/watch?v=ZVYGJYnJTi0• http://www.youtube.com/watch?v=S1Pi64I2wTU

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Slump

La Conchita, CA

Spring 1995

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RockslidePorteau 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, LaharMarch 21, 1982

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