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==Descrizione=

Il '''Dasht-e Lut''', talvolta scritto anche '''Dasht-i-Lut''', è un vasto [[deserto]] saltosalato dell'[[Iran]] sudorientale ed è il [[Deserti più grandi del mondo|venticinquesimo deserto più vasto del mondo]].

Climaticamente, l'Iran fa parte della fascia desertica afro-asiatica che va dalle isole di [[Capo Verde]], al largo dell'[[Africa Occidentale]] fino alla [[Mongolia]]. 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 {{convert|300|km|mi|sp=us}}. In near-tropical deserts, elevated areas capture most precipitation. As a result an [[abiotic]] zone.

Il '''Dasht-e Lut''', talvolta scritto anche '''Dasht-i-Lut''', è un vasto [[deserto]] salto dell'[[Iran]] sudorientale ed è il [[Deserti più grandi del mondo|venticinquesimo deserto più vasto del mondo]].

La geografia dell'Iran consiste in un [[altipiano iranico|altipiano]] circondato da montagne e diviso in bacini di drenaggio. Il Dasht-e-Lut, insieme al [[Dasht-e Kavir]], è uno dei più ampi di questi bacini, essendo lungo 480 km e largo 320 km<ref name="RD">{{cite book |

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 {{convert|300|km|mi|sp=us}}. In near-tropical deserts, elevated areas capture most precipitation. As a result an [[abiotic]] zone.

[[Geography of Iran|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, {{convert|480|km|mi|sp=us}} long and {{convert|320|km|mi|sp=us}} wide,<ref name="RD">{{cite book |

publisher = The Reader's Digest Association, Inc. |

title = Natural Wonders of the World |

Riga 19:

page = 117 |

author = editors, Richard L. Scheffel, Susan J. Wernert ; writers, Oliver E. Allen ... et al.}}

Larsuperficie</ref>, delcon desertouna èsuperficie di circa 51,.800 chilometri quadrati.<ref name=nyt>{{cite book |

</ref> and is considered to be one of the driest places on Earth.<ref name="csmonitor.com">http://www.csmonitor.com/2006/1102/p16s01-sten.html</ref><ref name="universetoday.com">http://www.universetoday.com/guide-to-space/earth/temperature-of-earth/</ref><ref name="redorbit.com">http://www.redorbit.com/images/images-of-the-day/img/13205/hottest_spot_on_earth/index.html</ref>

Larsuperficie del deserto è di circa 51,800 chilometri quadrati.<ref name=nyt>{{cite book |

first=John W. (ed.) |

last=Wright |

Riga 31 ⟶ 29:

isbn=978-0-14-303820-7 |

page=456}}

</ref>. andÈ isconsiderato considereduno todei beluoghi onepiù ofaridi thedel driest places on Earthpianeta.<ref name="csmonitor.com">http://www.csmonitor.com/2006/1102/p16s01-sten.html</ref><ref name="universetoday.com">http://www.universetoday.com/guide-to-space/earth/temperature-of-earth/</ref><ref name="redorbit.com">http://www.redorbit.com/images/images-of-the-day/img/13205/hottest_spot_on_earth/index.html</ref>

</ref> The other large basin is the [[Dasht-e Kavir]]. During the spring wet season, water briefly flows down from the [[Hazaran|Kerman mountains]], but it soon dries up, leaving behind only rocks, sand, and salt.

Durante la breve stagione umida, in primavera, l'acqua proveniente dalle montagne di [[Kerman]] inonda la zona, ma in breve tempo si prosciuga, lasciandosi dietro solo rocce, sabbia e sale.

TheLa easternparte partorientale ofdel Dasht-e Lut isè aun lowbasso plateaualtipiano coveredricoperto withda [[saltuno flat]]sstrato uniforme di sale. InAl contrastcontrario, theil centercentro hasè beenstato sculptedscolpito bydal thevento windin intouna aserie seriesdi ofcreste parallele ridgesavvallamenti and furrowsparalleli, extendingche oversi estendono per {{convert|150| km|mi|abbr=on}} ande reachingraggingono 75&nbsp;mi (250&nbsp;ft) inmetri di heightaltezza.<ref name="RD" /> ThisInoltre areain isquesta alsozona riddledsi withaprono [[ravine]]snumerosi gole anded [[sinkhole]]singhiottitoi. TheLa southeastparte issudorientale aè vastuna expansevasta ofdistesa sanddi sabbia, like a Saharansimile all'[[erg (landform)|erg]], withdel [[duneSahara]]s, su cui 300&nbsp;msorgono (1000&nbsp;ft)dune highalte fino a 300 metri, amongfra thele tallestpiù ingrandi theal worldmondo.<ref name="RD" />

== Più alta temperatura della superficie terrestre ==

== Hottest land surface ==

MeasurementsLe ofmisurazioni del MODIS ([[Moderate-Resolution Imaging Spectroradiometer]]) installedinstallato sul satellite ondella [[NASA]]'s satellite "[[Aqua (satellite)|Aqua]]" fromdal 2003 - 2005 testify that the hottest land surface on Earth ishanno locatedrilevato innel Dasht-e -Lut anduna landtemperatura surfacedella temperaturessperficie reachterestre heredi 70.7°C, degreesla Cpiù (159-160alta degreesmai F)registrata.<ref>http://earthobservatory.nasa.gov/IOTD/view.php?id=7149</ref><ref>http://www.weather.ir/english/</ref><ref>http://www.climatetemp.info/iran/</ref><ref>http://www.presstv.ir/Detail.aspx?id=58252&sectionid=351020108</ref><ref name="csmonitor.com"/><ref name="universetoday.com"/><ref name="redorbit.com"/>. PrecisionL'incertezza ofdella measurementsmisura isè di 0.,5 - 1 degreesgrado KKelvin<ref>http://modis.gsfc.nasa.gov/data/dataprod/dataproducts.php?MOD_NUMBER=11 MOD 11 - Land Surface Temperature and Emissivity, MODIS Website</ref><ref>http://modis.gsfc.nasa.gov/data/atbd/atbd_mod11.pdf Zhengming Wan, MODIS Land-Surface Temperature Algorithm Theoretical Basis Document (LST ATBD) Version 3.3. April 1999</ref>.

TheLa hottestzona partpiù ofcalda Dasht-edi Lutquesto isdeserto è Gandom Beryan -un approximatelypianoro 480coperto km²da largelava plateausolidificata coveredvasto withall'incirca dark480 km² lava<ref>http://www.iranreview.org/content/view/1067/51/ A Journey To Earth's Hottest Point</ref>. AccordingSecondo touna localleggenda legendlocale thisquesto namenome (che in translation from [[Persian language|PersianPersiano]] -significa "Toastedgrano wheattostato")deriva originatesda fromun anincidente accidenta whereseguito loaddel ofquale wheatun leftcarico indi thefrumento desertfu wasabbandonato scorchednel bydeserto, thevenendo heatbruciato indal acalore fewin dayspochi timegiorni<ref name="wond">{{Cite document |title = Gandom Beryan in Lut Desert - hottest place on Earth |publisher = Wondermondo |date = 1 November 2010 |url = http://www.wondermondo.com/Countries/As/Iran/Kerman/GandomBeryan.htm |postscript = <!-- Bot inserted parameter. Either remove it; or change its value to "." for the cite to end in a ".", as necessary. -->{{inconsistent citations}}}}</ref>.

==SeeVoci alsocorrelate==

*[[Dasht-e Kavir]]

*[[Geography ofGeografia dell'Iran]]

*[[International rankings of Iran]]

==ReferencesNote==

<references/>

==ExternalCollegamenti linksesterni==

{{commons|Dasht-e Lut}}

* [http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17226 NASA image and info]