Deserts of the world The Desert Biome Deserts World’s Largest Deserts Factmonster: Principal Deserts of the World North American Deserts Sonora Desert Sonoran Desert Southwest Deserts Great Basin Desert Mojave Desert The Chihuahuan Desert The Chihuahuan Desert Region Welcome to the Chihuahuan Desert The Chihuahuan Desert White Sands Desert of New mexico Deathe Valley Death Valley National Park OneWorld Magazine: Deserts of Our World Asian Deserts Middle Eastern/African Deserts Sahara Desert Sahara Desert Wadi Rum: Jordan South American Deserts Cold Deserts Siberia, Russia |
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يتبع…
Desert
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Area – sq miles
Africa
Sahara
Northern Africa
3,320,000
Libyan
Libya, Egypt, and Sudan (part of Sahara)
–
Kalahari
Southwestern Africa
360,000
Namib
Southwestern Africa
52,000
Asia
Arabia
Southwestern Asia
900,000
Rub’al Khali
southern Arabian Peninsula
250,000
Gobi
Mongolia and northeastern China
500,000
Kara-Kum
Turkmenistan
135,000
Kyzyl-Kum
Kazakhstan-Uzbekistan
115,000
Takla Makan
northern China
105,000
Kavir
central Iran
100,000
Syrian
Saudi Arabia, Jordan, Syria, and Iraq
100,000
Thar
India and Pakistan
77,000
Dasht-e-Lut
eastern Iran
20,000
Australia
Great Victoria
Western and South Australia
250,000
Great Sandy
northern Western Australia
150,000
Gibson
Western Australia
–
Simpson
Northern Territory
56,000
North America
Great Basin
southwestern United States
190,000
Chihuahuan
northern Mexico
175,000
Sonoran
southwestern U.S. and Baja California
120,000
Colorado
California and northern Mexico
–
Yuma
Arizona and Sonora, Mexico
–
Mojave
southwestern United States
25,000
South America
Patagonian
southern Argentina
260,000
Atacama
northern Chile
54,000
يتبع …
A desert is a landscape form or region that receives very little precipitation
Deserts are defined as areas that receive an average annual precipitation of less than 250
mm (10 in). In the Köppen climate classification system, deserts are classed as (BW).
مقدمه
Geography
A satellite image of the Sahara, the world’s largest hot desert and second largest desert after Antarctica.
Deserts take up one-third of the Earth’s land surface.[1] They usually have a large diurnal and seasonal temperature range, with high daytime temperatures (in summer up to 45 °C or 113 °F), and low night-time temperatures (in winter down to 0 °C; 32 °F) due to extremely low humidity. Water acts to trap infrared radiation from $$$$ the sun and the ground, and dry desert air is incapable of blocking sunlight during the day or trapping heat during the night. Thus during daylight most of the sun’s heat reaches the ground. As soon as the sun sets the desert cools quickly by radiating its heat into space. Urban areas in deserts lack large (more than 25 °F/14 °C) daily temperature ranges, partially due to the urban heat island effect.
Many deserts are formed by rain shadows, mountains blocking the path of precipitation to the desert. Deserts are often composed of sand and rocky surfaces. Sand dunes called ergs and stony surfaces called hamada surfaces compose a minority of desert surfaces. Exposures of rocky terrain are typical, and reflect minimal soil development and sparseness of vegetation.
The snow surface at Dome C Station in Antarctica is a representative of the majority of the continent’s surface.
Bottomlands may be salt-covered flats. Eolian processes are major factors in shaping desert landscapes. Cold deserts (also known as polar deserts) have similar features but the main form of precipitation is snow rather than rain. Antarctica is the world’s largest cold desert (composed of about 98 percent thick continental ice sheet and 2 percent barren rock). The largest hot desert is the Sahara.
Deserts sometimes contain valuable mineral deposits that were formed in the arid environment or that were exposed by erosion. Because deserts are so dry, they are ideal places for artifacts and fossils to be preserved.
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Deserts of the world
مواقع بتفيييدكم ان شاء الله منقووووووول Principal Deserts of the World — Infoplease.com |
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