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Deserts
. Background for the Teacher »
. Spreading Desert »
. Climate Change »
. Effects of Desertification »
. Skills Developed »
. Combating
Desertification
 »
. Fast Facts »
. Internet Activity »
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. Deserts of the world »
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  Enjoy the earth gently for if it is spoiled it cannot be repaired.

 

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Teacher's Sheet = Teacher's
Student's Sheet = Student's
   
 
Teacher'sActivity 1:
Student's
Planting Trees to Hold Back the Desert?  
   
 
Teacher'sActivity 2:
Student's
What is Soil?
   
 
Teacher'sActivity 3:
Student's
The Importance of Plant Cover
   
 
Teacher'sActivity 4:
Student's
Take Action Around the World
   
 

Deserts

The Earth's land surface is divided into zones or biomes. These biomes are designated according to climate and other physical characteristics. Each biome has a distinctive combination of life forms that are able to thrive in the particular conditions found there. Desert is one biome. Others include: tundra, boreal forest, tropical rainforest, savanna and mountain.

A desert is defined as an area that receives 25 cm of rain or less a year. Natural deserts are part of the world's arid zones. Arid means that the land is dry and barren. These lands, together with the semi-arid lands that surround them, cover one-third of the Earth's surface. Some deserts form in large land masses in the interior of a country. This is because after the wind has traveled a great distance inland from the coast, it has lost all its moisture. Other deserts form on the far side of mountain ranges because there is no rain left in the clouds once they reach the interior of the mountain range.

With little rain and extreme temperatures (very hot and very cold), deserts can be the driest places in the world. Deserts occur naturally all over the globe, but most are found near the Tropic of Cancer and the Tropic of Capricorn. This is where the sun is very strong and wind patterns produce many cloudless days. Without clouds, there is nothing to shield the ground from the sun. During the summer, the ground can bake from the heat. The desert floor also becomes very cold at night when the heat is lost back to the atmosphere. Temperatures in the desert range from 25ºC in the shade to the low 40ºC range in the sun. (There are also cold deserts like the Antarctic, which are covered with snow and ice all of the time.)

Deserts are often portrayed as vast areas of blowing sand. This isn't always the case. There are also deserts made of gravel, bare rock and boulders. Desert sand starts out as rock, but over time, it is weathered down to form fine particles of sand. Various sand dunes form as a result of the blowing winds, creating different shapes such as ridges, stars and crescents.

There are many living things that survive in the desert including human beings, animals and plants. They have learned to adapt to the harsh climate. For example, the hard outer shell of a scorpion helps reduce water loss. And when the sun becomes too hot, the Kalahari desert ground squirrel uses its tail like an umbrella to protect it from the hot sun.

The camel, an animal that is often associated with the desert, has many physical adaptations that allow it to survive and act as a mode of transportation for humans living in the desert. Camels have few sweat glands and are able to conserve water because their body temperature can rise several degrees before they start to sweat. They can also survive for long periods without food by using the fat stored in their humps.

Desert plants, such as cacti, are able to store water more easily because of their thick, waxy outer layer that protects the plant from the intense sun. Some plants have long roots to reach water located deep in the soil; others spread their roots to gather water over a wide area, and some absorb dew through their leaves.

People, too, have learned to live in the desert. Some are nomads, which means they move from place to place when their livestock need new pasture. Others live in permanent dwellings such as mud huts, well adapted to local conditions.

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