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Dasht-e Lut

Coordinates: 30°36′18″N 59°04′04″E / 30.60500001°N 59.0677777878°E / 30.60500001; 59.0677777878
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As seen from space
Map of biotopes of Iran
  Forest steppe
  Forests and woodlands
  Semi-desert
  Desert lowlands
  Steppe
  Salted alluvial marshes

Dasht-e Lut, also spelled Dasht-i-Lut, is a large salt desert in southeastern Iran and is the world's 25th largest desert.

Iran is climatically part of the Afro-Asian belt of deserts that stretch from the Cape Verde islands off West Africa all the way to Mongolia near Beijing, China. The patchy, elongated, light-colored feature in the foreground (parallel to the mountain range) is the northernmost of the Dasht dry lakes that stretch southward 300 kilometers (186 miles). In near-tropical deserts, elevated areas capture most precipitation. As a result, the Dasht-e Lut is generally considered to be an abiotic zone.

Iran's geography consists of a plateau surrounded by mountains and divided into drainage basins. Dasht-e Lut is one of the largest of these desert basins, 480 kilometers (300 miles) long and 320 kilometers (200 miles) wide,[1] and is also the hottest and driest place on earth.[2][3][4] This region which covers an area of about 480 square kilometers is called Gandom Beriyan (the toasted wheat). Its surface is wholly matted with black volcano lava. This dark cover absorbs excessive sunshine which due to difference of temperature with neighboring elevations forms a wind tunnel. There are reports that no living creature lives in this region.[citation needed] Dasht-e Lut has an area of about 51,800 square kilometers (20,000 mi²).[5] The other large basin is the Dasht-e Kavir. During the spring wet season, water briefly flows down from the Kerman mountains, but it soon dries up, leaving behind only rocks, sand, and salt.

The eastern part of Dasht-e Lut is a low plateau covered with salt flats. In contrast, the center has been sculpted by the wind into a series of parallel ridges and furrows, extending over 150 km (90 miles) and reaching 75 m (250 ft) in height.[1] This area is also riddled with ravines and sinkholes. The southeast is a vast expanse of sand, like a Saharan erg, with dunes 300 m (1000 ft) high, among the tallest in the world.[1]

Climate

The highest temperature of Earth's surface in the years 2004 and 2005 was found to be in Dasht-e Lut with a temperature of 70.7 degrees C (159 degrees F), recorded by MODIS of NASA.[6][7][8][9][2][3][4]. This sensor does not measure air temperature but rather temperature of the surface itself, which can be considerably higher. Temperatures at night time in the summer could be above 40 Degrees C (104 Degrees F), while daytime air temperatures above 50 degrees C (120 degrees F) are very common.[citation needed]

See also

References

  1. ^ a b c editors, Richard L. Scheffel, Susan J. Wernert ; writers, Oliver E. Allen ...; et al. (1980). Natural Wonders of the World. The Reader's Digest Association, Inc. p. 117. ISBN 978-0-89577-087-5. {{cite book}}: |author= has generic name (help); Explicit use of et al. in: |author= (help)CS1 maint: multiple names: authors list (link)
  2. ^ a b http://www.csmonitor.com/2006/1102/p16s01-sten.html
  3. ^ a b http://www.universetoday.com/guide-to-space/earth/temperature-of-earth/
  4. ^ a b http://www.redorbit.com/images/images-of-the-day/img/13205/hottest_spot_on_earth/index.html
  5. ^ Wright, John W. (ed.) (2006). The New York Times Almanac (2007 ed.). New York, New York: Penguin Books. p. 456. ISBN 978-0-14-303820-7. {{cite book}}: |first= has generic name (help)
  6. ^ http://earthobservatory.nasa.gov/IOTD/view.php?id=7149
  7. ^ http://www.weather.ir/english/
  8. ^ http://www.climatetemp.info/iran/
  9. ^ http://www.presstv.ir/Detail.aspx?id=58252&sectionid=351020108

30°36′18″N 59°04′04″E / 30.60500001°N 59.0677777878°E / 30.60500001; 59.0677777878