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3.2 WIND EROSION AND DEPOSITION Kavya, Olga, Ivy, and Grace

3.2 Wind Erosion and Deposition

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3.2 Wind Erosion and Deposition. Kavya, Olga, Ivy, and Grace. Questions For You!!!. What are the three different processes of erosion by wind? Why is loess found very far away from its source?. Fun Facts. Wind erosion causes more than half of the soil loss in the U.S.A. per year. - PowerPoint PPT Presentation

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Page 1: 3.2 Wind Erosion  and Deposition

3.2 WIND EROSION AND

DEPOSITION

Kavya, Olga, Ivy, and Grace

Page 2: 3.2 Wind Erosion  and Deposition

Questions For You!!!

• What are the three different processes of erosion by wind?

• Why is loess found very far away from its source?

Page 3: 3.2 Wind Erosion  and Deposition

FUN FACTS Wind erosion causes more than half of the

soil loss in the U.S.A. per year. In the Great Plains, five million acres are

damaged by wind erosion annually. Landmarks such as Bryce Canyon, the Grand

Canyon, and others are formed partially by wind erosion.

Page 4: 3.2 Wind Erosion  and Deposition

THE PROCESS OF WIND EROSION

Saltation is the movement of sand or other sediments by short jumps and bounces that is caused by wind or water.

Deflation is a form of wind erosion in fine, dry soil particles are blown away.

Abrasion is the grinding and wearing away of rock surfaces through the mechanical action of other rock or sand particles.

Page 5: 3.2 Wind Erosion  and Deposition

SALTATION When moving sand grains hit each other it

causes other grains of sand to bounce up or fall forward.

Page 6: 3.2 Wind Erosion  and Deposition

DEFLATION

Wind removes the top layer of sediment and leaves behind the larger, heavier pieces of rock.

In areas where there are few plants the wind may scoop out depressions in the landscape. These depressions are called deflation hollows.

Page 7: 3.2 Wind Erosion  and Deposition

ABRASION

Abrasion occurs most often in areas where there are strong winds, loose sands, and soft rocks.

When the wind picks up millions of sharp sand grains it creates a sandblasting effect. This effect helps to erode and smooth rocks.

Page 8: 3.2 Wind Erosion  and Deposition

WIND DEPOSITED MATERIALS

Vocabulary• Loess- very fine sediments deposited by wind

•Dune- a mound of wind-deposited sand that keeps its shape even though it moves

Page 9: 3.2 Wind Erosion  and Deposition

LOESS

Because wind carries fine-grained material much higher and further than it carries sand, loess deposits are sometimes found far away from their source.

Page 10: 3.2 Wind Erosion  and Deposition

DUNESDUNES

1)1) When the wind hits an obstacle, such as a When the wind hits an obstacle, such as a plant or rock, it slows and drops heavier plant or rock, it slows and drops heavier materials.materials.

2)2) The material collects creating a new The material collects creating a new obstacle which causes even more material obstacle which causes even more material to be deposited, forming a mound. The to be deposited, forming a mound. The original obstacle is eventually buried. original obstacle is eventually buried.

3)3) These mounds are called dunes and are These mounds are called dunes and are commonly found in sandy deserts and commonly found in sandy deserts and along the shores of lakes and oceans.along the shores of lakes and oceans.

Page 11: 3.2 Wind Erosion  and Deposition

THE MOVEMENT OF DUNES

Dunes move in the direction of strong winds. The gently sloped side faces the wind, which

constantly transports material up this side. As sand moves over the crest, or peak, of the

dune, it slides down the slip face, creating a steep slope.

Page 12: 3.2 Wind Erosion  and Deposition

ANSWERS FOR YOUQ: What are the three different processes of

erosion by wind?A: Saltation, Deflation, and Abrasion.

Q: Why is loess found very far away from its source?

A: Because wind carries fine-grained material (loess) much higher and further than it carries sand.

Page 13: 3.2 Wind Erosion  and Deposition