Top Banner
DESERTS
24
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Deserts

DESERTS

Page 2: Deserts

What is a desert?

What do deserts look like?

What makes a desert?

Where are deserts found?

Page 3: Deserts

Deserts can be found all over the world.

Page 4: Deserts

Deserts are the most brutal areas here on Earth. Their most fundamental characteristic is a

shortage of available moisture for plants, resulting from an imbalance between precipitation and evaporation. Which means they can frequently lose more moisture through evaporation than they receive from annual precipitation.

Dry soil becomes sensitive to erosion processes which carries sand and shapes rocks, creating a beautiful but unwelcoming landscapes.

Page 5: Deserts
Page 6: Deserts

Types of deserts

Subtropical deserts

Continental deserts

Cold winter deserts

Coastal deserts

Page 7: Deserts

Sahara of Northern Africa, Kalhari of Southern Africa, and the Great Australian Desert.

Subtropical deserts

Page 8: Deserts

Gobi, Takla Makan

Continental deserts

Page 9: Deserts

Deserts east of the Sierra Nevada Mountains, California & Nevada, East of the Cascades of Oregon and Washington, and East of the Andes Mountains in South America.

Cold winter deserts

Page 10: Deserts

Atacama Desert of coastal Peru, Namib Desert of coastal South Africa.

Coastal deserts

Page 11: Deserts

Northern Greenland, and ice- free areas of Antarctica.

Polar deserts

Page 12: Deserts

Desert surfaces

Sand covers only about 20% of desert surfaces, most of it in vast sand sheets and sand seas.

Page 13: Deserts

Desert surfaces

Hamadas are relatively level plains that are covered by boulders and exposed bedrock.

Page 14: Deserts

Aeolian processes

Erosion is the process by which soil and rock are removed from the Earth's surface by exogenic processes such as wind or water flow, and then transported and deposited in other locations.

Page 15: Deserts

Aeolian processes

Wadi is the Arabic term that refers to a valley. In some cases it can also refer to a dry riverbed that only experiences water when there is a heavy rain fall.

Page 16: Deserts

Aeolian processes

A mushroom rock, also called a pedestal rock, is a naturally occurring rock whose shape, as its name implies, strikingly resembles a mushroom.

Page 17: Deserts

Aeolian processes

A yardang is a streamlined hill carved from bedrock by the dual action of wind abrasion, and deflation.

Page 18: Deserts

Aeolian processes

Tafoni are small cave-like features found in granular rock such as sandstone, with rounded entrances and smooth concave walls, often connected.

Page 19: Deserts

Dunes

Wind plays an important role in deserts. It moves large amounts of soil around, covering much of the world's deserts with sand. About half of the sand fields of hot deserts exist as sand dunes.

A dune is a hill of sand built by either wind or water flow.

The shapes and sizes of dunes change constantly, but they can be grouped into a few simple categories: linear, star, and barkhan dunes.

Page 20: Deserts

Linear (longitudinal) dunes

Dunes

Page 21: Deserts

Star dunes

Dunes

Page 22: Deserts

Crescent sand dunes, also called barkhan or transverse

Dunes

Page 23: Deserts

At first glance, it may seem as there is not much in a desert. The land may seem empty. The quiet suggests that there are few or no animals. The weather may not seem friendly to life. But if we look closer, a desert is made of ecosystems. In an ecosystem, plants, animals, land, water and air work together.

Deserts can be filled with life!

Page 24: Deserts

Thank you for attention!

Igor Nemanjić