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Published byMilko Pretnar Modified over 6 years ago
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Wind Most common in dry regions 2 main forms Deflation
Abrasion (sandblasting)
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Deflation Wind blows away small loose sediments
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Sandblasting or Abrasion
Wind blows sand or silt grains against other rocks More effective at lower heights Results in an appearance that is Frosted Pitted
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Erosion by Glaciers Glacier
Naturally formed mass of ice or snow that moves downhill due to gravity
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Types of Glaciers Mountain Glaciers Continental Glaciers
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Glacial Movement Glacial advance Glacial retreat
More snow & ice accumulate than melt Glacial retreat Melting occurs faster than the snow & ice are added
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Characteristics of Glacial Erosion
Grooves and scratches in the rock Erratics Large sediment that seem out of place
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U-Shaped Valleys Rocky River, Jasper National Park, Alberta.
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Glacial Landscape Features
Horn Cirque Bowl-shaped Basins
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Matterhorn
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Waves and Current Erosion
Waves are energy disturbances in water Caused by: Wind Fetch Distance the wind blows on the water
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Longshore Current Waves hit the beach at an angle
Net result is movement of the sand in one direction
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Jetties Structures built to slow sand movement
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Shoreline Erosion Breakwater Built to try and slow erosion
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Coastline Features Barrier Beach Spit Extension of sand
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Human Causes of Erosion
Construction Mining Deforestation Overgrazing Poor farming methods
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