Unit 5: Gradational Processes Ms. Thind. revision/geography/development/case-...

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WIND EROSION AND LANDFORMS OF DESERT AREAS Unit 5: Gradational Processes Ms. Thind

Transcript of Unit 5: Gradational Processes Ms. Thind. revision/geography/development/case-...

Page 1: Unit 5: Gradational Processes Ms. Thind.   revision/geography/development/case- studies/case-study-sahel-desertification.

WIND EROSION AND LANDFORMS OF DESERT AREAS

Unit 5: Gradational ProcessesMs. Thind

Page 2: Unit 5: Gradational Processes Ms. Thind.   revision/geography/development/case- studies/case-study-sahel-desertification.

DESERTIFICATION

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http://revisionworld.com/gcse-revision/geography/development/case-studies/case-study-sahel-desertification

Page 5: Unit 5: Gradational Processes Ms. Thind.   revision/geography/development/case- studies/case-study-sahel-desertification.
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THE DESERT

: an area in which the annual rainfall is not sufficient to maintain a continuous cover of vegetation.

: wind has an opportunity to play a major part in the creation of desert landforms.

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WHY…

few plants to anchor the debris and little vegetation to restrict air movements = winds of the desert are able to whip up rock fragments and carry them formation of distinct landforms.

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WHERE ARE THE WORLDS DESERTS?

1. Sahara Desert2. Arabian Desert3. Gobi Desert4. Syrian Desert5. Great Basin Desert 6. Patagonian Desert7. Kalahari Desert8. Great Victorian Desert

Label the following 8 deserts on your map.

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DESERTS OF THE WORLD

Equator

COC

COC

COC

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DESERTS AND WIND ACTION

Strong winds carry light surface materials are carried by suspension.

Movement of sand in the desert is largely by saltation: particles roll and bounce along the ground.

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Moving sand can have an abrasive power on existing landforms.

Strongest close to the ground and create features called toadstools.

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DEFLATION

Refers to wind blowing away sand, silt and clay in deserts so that underlying rocks become exposed.

The resulting landforms are deep hollows called blowouts and stony landscapes called Badlands.

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SAND DUNES

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DUNE FORMATION

Winds carry sand over the desert landscape deposits of sand collect on some obstruction over time a sand dune will take shape.

Long, gentle slope on windward side and steep slope on leeward side slip face.

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DUNE MIGRATION

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BARCHANS

- Crescent shaped - Forms over small

boulder - Horns point

downwind - Sand blows up the

windward slope and slides down the slip face

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TRANSVERSE DUNES

- Abundant sand needed

- Continuous sand ridge forms at right angles to wind

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PARABOLIC

- Crescent shaped - Horns point up

wind - Vegetation

anchors the horns

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LONGITUDINAL DUNES

Found in deserts where only a thin layer of sand is present

- Winds blow continuously in one direction

- Long and straight parallel to the wind

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UNIQUE LANDFORMS

Alluvial Fans Playa lakes Canyons Plateau Buttes Mesa Ergs