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Deserts in the World

A desert is a barren area of the landscape where little precipitation occurs and consequently, living conditions are hostile for plant and animal life. The lack of vegetation exposes the unprotected surface of the ground to the processes of denudation. About one-third of the land surface of the world is arid or semi-arid. This includes much of the polar regions where little precipitation occurs and which are sometimes called polar deserts or “cold deserts”. Deserts can be classified by the amount of precipitation that falls, by the temperature that prevails, by the causes of desertification or by their geographical location.

Deserts are formed by weathering processes as large variations in temperature between day and night put strains on the rocks which consequently break in pieces. Although rain seldom occurs in deserts, there are occasional downpours that can result in flash floods. Rain falling on hot rocks can cause them to shatter and the resulting fragments and rubble strewn over the desert floor is further eroded by the wind. This picks up particles of sand and dust and wafts them aloft in sand or dust storms. Wind-blown sand grains striking any solid object in their path can abrade the surface. Rocks are smoothed down, and the wind sorts sand into uniform deposits. The grains end up as level sheets of sand or are piled high in billowing sand dunes. Other deserts are flat, stony plains where all the fine material has been blown away and the surface consists of a mosaic of smooth stones. These areas are known as desert pavements and little further erosion takes place. Other desert features include rock outcrops, exposed bedrock and clays once deposited by flowing water. Temporary lakes may form and salt pans may be left when waters evaporate. There may be underground sources of water in the form of springs and seepages from aquifers. Where these are found, oases can occur.

Plants and animals living in the desert need special adaptations to survive in the harsh environment. Plants tend to be tough and wiry with small or no leaves, water-resistant cuticles and often spines to deter herbivory. Some annual plants germinate, bloom and die in the course of a few weeks after rainfall while other long-lived plants survive for years and have deep root systems able to tap underground moisture. Animals need to keep cool and find enough food and water to survive. Many are nocturnal and stay in the shade or underground during the heat of the day. They tend to be efficient at conserving water, extracting most of their needs from their food and concentrating their urine. Some animals remain in a state of dormancy for long periods, ready to become active again when the rare rains fall. They then reproduce rapidly while conditions are favourable before returning to dormancy.

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Here we have listed Important Deserts of the world which are regularly been asked in SSC and Banking Exams under General Awareness section.

List of Important Deserts in the World:

Continent Desert Name Type of Desert Position
Antarctica Antarctic Polar South Pole
Asia, Europe & North America Arctic Polar North Pole
Asia Kara Kum Cold Winter Central Asia
Kyzyl Kum Cold Winter Kazakhstan & Uzbekistan
Gobi Cold Winter Mongolia
Taklamakan Cold Winter China
Thar-Cholistan Subtropical India and Pakistan
Africa Kalahari Subtropical Southern Africa
Namib Cool Coastal Southern Africa
Sahara Subtropical Northern Africa
Australia Gibson Subtropical Central Australia
Great Sandy Subtropical North-Western Australia
Great Victoria Subtropical Central Australia
Simpson Subtropical Central Australia
Tanami Subtropical Northern Australia
Europe Arabian Subtropical Arabian Peninsula
Dasht-e Kavir Subtropical Central Iran
Dasht-e Lut Subtropical Southeastern Iran
North America Chihuahuan Subtropical North America
Great Basin Cold Winter US
Mojave Subtropical US
Sonoran Subtropical North America
South America Atacama Cool Coastal Chile
Patagonian Cold Winter Southern Part of South America