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	<title>Murzuq Desert - Revision history</title>
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		<title>imported&gt;Salmoonlight at 20:32, 1 March 2025</title>
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		<updated>2025-03-01T20:32:27Z</updated>

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&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{Short description|Sandy desert in Libya}}&lt;br /&gt;
{{Infobox settlement&lt;br /&gt;
| name                    = Idehan Murzuq&lt;br /&gt;
| native_name             = {{lang|ar|أدهان مرزق}}&lt;br /&gt;
| native_name_lang        = &amp;lt;!-- ISO 639-2 code e.g. &amp;quot;fr&amp;quot; for French. If more than one, use {{lang}} instead --&amp;gt;&lt;br /&gt;
| settlement_type         = [[Erg]]&lt;br /&gt;
| image_skyline           =Sanddunes marzuq sandsea.jpg&lt;br /&gt;
| image_alt               = &lt;br /&gt;
| image_caption           =Marzuq Sand Sea seen from [[International Space Station|ISS]], 2008 (centered at {{Coord|24.5|N|12|E|display=inline}}). Detailed [[astronaut]] photograph, taken from [[low Earth orbit]], showing classic large and small sand masses of the central Sahara where wind is a more powerful land-shaping agent than water. &lt;br /&gt;
| image_flag              = &lt;br /&gt;
| flag_alt                = &lt;br /&gt;
| image_seal              = &lt;br /&gt;
| seal_alt                = &lt;br /&gt;
| image_shield            = &lt;br /&gt;
| shield_alt              = &lt;br /&gt;
| nickname                = &lt;br /&gt;
| motto                   = &lt;br /&gt;
| image_map               =Saharan topographic elements map.png&lt;br /&gt;
| map_alt                 = &lt;br /&gt;
| map_caption             =Map of the topographic features of the Sahara&lt;br /&gt;
| pushpin_map             = &lt;br /&gt;
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| pushpin_map_alt         = &lt;br /&gt;
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| coordinates             = {{coord|24|45|N|13|00|E|display=inline,title|region:MR_type:city_source:GNS-enwiki}}&lt;br /&gt;
| coor_pinpoint           = &lt;br /&gt;
| coordinates_footnotes   = &lt;br /&gt;
| subdivision_type        = Country&lt;br /&gt;
| subdivision_name        = [[Libya]]&lt;br /&gt;
| subdivision_type1       = &lt;br /&gt;
| subdivision_name1       = &lt;br /&gt;
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| area_total_km2          = 58000&lt;br /&gt;
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| elevation_footnotes     = &lt;br /&gt;
| elevation_m             = 660&lt;br /&gt;
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| population_density_km2  = auto&lt;br /&gt;
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| website                 = &amp;lt;!-- {{URL|example.com}} --&amp;gt;&lt;br /&gt;
| footnotes               =  &lt;br /&gt;
}}&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Murzuq Desert&amp;#039;&amp;#039;&amp;#039;, &amp;#039;&amp;#039;&amp;#039;Idehan Murzuq&amp;#039;&amp;#039;&amp;#039;, or &amp;#039;&amp;#039;&amp;#039;Idhan Murzuq&amp;#039;&amp;#039;&amp;#039; (also Murzaq, Murzuk, Marzuq and Murzak), is an [[Erg (landform)|erg]] in southwestern [[Libya]] with a surface of approximately 58,000 km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;.&amp;lt;ref&amp;gt;[https://books.google.com/books?id=WOcUNbRUGtwC&amp;amp;dq=%22Desert+Geomorphology%22+great+sand+sea&amp;amp;pg=PA403 Desert Geomorphology, p. 403]&amp;lt;/ref&amp;gt; It is named after the town of [[Murzuk]] in the [[Fezzan]] region. Like the [[Idehan Ubari]] further north, the Idehan Murzuq is part of the greater [[Sahara Desert]] region. It is separated from the southern Sahara Desert by the [[Tibesti Mountains]] and the [[Tassili n&amp;#039;Ajjer]].&lt;br /&gt;
&lt;br /&gt;
==Dune pattern==&lt;br /&gt;
The &amp;#039;&amp;#039;“Draa”&amp;#039;&amp;#039; [[dunes]] (from the [[Arabic]] for “arm”) are very large masses of sand in the western part of Libya&amp;#039;s vast  Murzuq Desert, and they appear in satellite images as a broad network of yellow-orange sand masses, with smooth-floored, almost sand-free basins between them. Geologists think that the &amp;#039;&amp;#039;draa&amp;#039;&amp;#039; of the Marzuq were probably formed by winds different from the prevailing north-northeast winds of today.&lt;br /&gt;
&lt;br /&gt;
Numerous smaller dunes have developed on the backs of the &amp;#039;&amp;#039;draa&amp;#039;&amp;#039;. Three distinct dune types are visible in satellite images of the region: &lt;br /&gt;
*[[Dunes#Longitudinal (Seif) and transverse dunes|Longitudinal dunes]], more or less parallel with the north winds.&lt;br /&gt;
*[[Dunes#Longitudinal (Seif) and transverse dunes|Transverse dunes]], usually more curved and formed at right angles to the wind.&lt;br /&gt;
*[[Dunes#Star|Star dunes]], in which several linear arms converge towards a single peak.&lt;br /&gt;
&lt;br /&gt;
The upwind sides of the sand masses appear smoother than the downwind side. Wind is moving sand grains almost all the time. This means that the &amp;#039;&amp;#039;draa&amp;#039;&amp;#039; and the dunes are all moving as sand is added on the upwind side and blown off the downwind side. Small sand masses move much faster than large sand masses. &lt;br /&gt;
&lt;br /&gt;
The &amp;#039;&amp;#039;draa&amp;#039;&amp;#039; are almost stationary, but the smaller dunes move relatively quickly across their backs. When the smaller dunes reach the downwind side of the &amp;#039;&amp;#039;draa&amp;#039;&amp;#039;, they are obliterated; their sand is blown across the basins as individual grains.&amp;lt;ref&amp;gt;[http://earthobservatory.nasa.gov/IOTD/view.php?id=36675 Sand Dunes, Marzuq Sand Sea, Southwest Libya.] This article incorporates [[public domain]] text from this [[NASA]] website.&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==Petroleum==&lt;br /&gt;
Since oil exploration began in 1957, eleven oil fields, including [[Nc186|NC186]], have been discovered in the Murzuq Basin. Two of the fields are considered giants, and altogether there are more than 2 billion barrels of oil in reserves under the desert there.&amp;lt;ref&amp;gt;Rusk, Donald C. (2001) &amp;quot;Libya:Petroleum Potential of the Underexplored Basin Centers &amp;amp;ndash; A Twenty-First-Century Challenge&amp;quot; &amp;#039;&amp;#039;In&amp;#039;&amp;#039; Downey, Marlan W.; Threet, Jack C. and Morgan, William A. (2001) &amp;#039;&amp;#039;Petroleum Provinces of the Twenty-first Century&amp;#039;&amp;#039; (AAPG Memoir 74) American Association of Petroleum Geologists, Tulsa, Oklahoma, pp. 429-452, p. 429, {{ISBN|0-89181-355-1}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
*[[Geography of Libya]]&lt;br /&gt;
*[[List of ergs]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
&lt;br /&gt;
==External links==&lt;br /&gt;
{{Commons-inline|Murzuq Desert}}&lt;br /&gt;
*[http://eol.jsc.nasa.gov/Collections/EarthObservatory/articles/MarzuqSandSeaLibya.htm View of the entire Murzuq Desert seen from the International Space Station]&lt;br /&gt;
&lt;br /&gt;
[[Category:Deserts of Libya]]&lt;br /&gt;
[[Category:Fezzan]]&lt;br /&gt;
[[Category:Ergs of Africa]]&lt;br /&gt;
[[Category:Sahara]]&lt;/div&gt;</summary>
		<author><name>imported&gt;Salmoonlight</name></author>
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