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Wind Most common in dry regions 2 main forms Deflation

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Presentation on theme: "Wind Most common in dry regions 2 main forms Deflation"— Presentation transcript:

1 Wind Most common in dry regions 2 main forms Deflation
Abrasion (sandblasting)

2 Deflation Wind blows away small loose sediments

3 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

4 Erosion by Glaciers Glacier
Naturally formed mass of ice or snow that moves downhill due to gravity

5 Types of Glaciers Mountain Glaciers Continental Glaciers

6 Glacial Movement Glacial advance Glacial retreat
More snow & ice accumulate than melt Glacial retreat Melting occurs faster than the snow & ice are added

7 Characteristics of Glacial Erosion
Grooves and scratches in the rock Erratics Large sediment that seem out of place

8 U-Shaped Valleys Rocky River, Jasper National Park, Alberta.

9 Glacial Landscape Features
Horn Cirque Bowl-shaped Basins

10 Matterhorn

11 Waves and Current Erosion
Waves are energy disturbances in water Caused by: Wind Fetch Distance the wind blows on the water

12 Longshore Current Waves hit the beach at an angle
Net result is movement of the sand in one direction

13 Jetties Structures built to slow sand movement

14 Shoreline Erosion Breakwater Built to try and slow erosion

15 Coastline Features Barrier Beach Spit Extension of sand

16 Human Causes of Erosion
Construction Mining Deforestation Overgrazing Poor farming methods


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