<?xml version="1.0"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="en">
	<id>https://en.bharatpedia.org/w/index.php?action=history&amp;feed=atom&amp;title=Mantle_%28geology%29</id>
	<title>Mantle (geology) - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://en.bharatpedia.org/w/index.php?action=history&amp;feed=atom&amp;title=Mantle_%28geology%29"/>
	<link rel="alternate" type="text/html" href="https://en.bharatpedia.org/w/index.php?title=Mantle_(geology)&amp;action=history"/>
	<updated>2026-08-20T00:41:43Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.43.6</generator>
	<entry>
		<id>https://en.bharatpedia.org/w/index.php?title=Mantle_(geology)&amp;diff=309417&amp;oldid=prev</id>
		<title>ImportMaster: robot: Creating new article from Special:WantedPages</title>
		<link rel="alternate" type="text/html" href="https://en.bharatpedia.org/w/index.php?title=Mantle_(geology)&amp;diff=309417&amp;oldid=prev"/>
		<updated>2022-02-23T23:20:46Z</updated>

		<summary type="html">&lt;p&gt;robot: Creating new article from &lt;a href=&quot;/wiki/Special:WantedPages&quot; title=&quot;Special:WantedPages&quot;&gt;Special:WantedPages&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;A &amp;#039;&amp;#039;&amp;#039;mantle&amp;#039;&amp;#039;&amp;#039; is a layer inside a [[Planet|planetary body]] that is between the [[core]] and the [[Crust (geology)|crust]] of a planetary body. Mantles are made of [[Rock (geology)|rock]] or [[Ice|ices]]. They are generally the largest layer of the planetary body. All [[Terrestrial planet|terrestrial planets]], a number of [[Asteroid|asteroids]], and some [[moons]] have mantles.&lt;br /&gt;
&lt;br /&gt;
== Earth&amp;#039;s mantle ==&lt;br /&gt;
{{Main|Earth&amp;#039;s mantle}}&lt;br /&gt;
The Earth&amp;#039;s mantle is a layer of [[silicate]] rock between the crust and the outer core. Its [[mass]] is 4.01 × 10&amp;lt;sup&amp;gt;24&amp;lt;/sup&amp;gt; kg. It makes up 67% the mass of the Earth. It has a thickness of 2,900&amp;amp;nbsp;kilometres (1,800&amp;amp;nbsp;mi).&amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;{{cite book|url=https://www.worldcat.org/oclc/65171709|title=The planetary scientist&amp;#039;s companion|last=Lodders, Katharina.|date=1998|publisher=Oxford University Press|others=Fegley, Bruce.|isbn=978-1-4237-5983-6|location=New York|oclc=65171709}}&amp;lt;/ref&amp;gt; It makes up about 84% of Earth&amp;#039;s [[volume]]. The Earth&amp;#039;s mantle behaves as a [[Viscosity|viscous]] [[fluid]].&lt;br /&gt;
&lt;br /&gt;
== Other planetary mantles ==&lt;br /&gt;
[[Mercury (planet)|Mercury]] has a silicate mantle that is [[approximately]] 490&amp;amp;nbsp;km thick. Mercury&amp;#039;s mantle makes up 28% of its mass. [[Venus|Venus&amp;#039;s]] silicate mantle is approximately 2800&amp;amp;nbsp;km thick. Venus&amp;#039;s mantle makes up around 70% of its mass. [[Mars|Mars&amp;#039;s]] silicate mantle is approximately 1600&amp;amp;nbsp;km thick. Mar&amp;#039;s mantle makes up 74–88% of its mass.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Moons with mantles ==&lt;br /&gt;
Jupiter&amp;#039;s moons [[Io (moon)|Io]], [[Europa (moon)|Europa]], and [[Ganymede (moon)|Ganymede]] have silicate mantles. Io&amp;#039;s mantle is 1100&amp;amp;nbsp;km thick. Ganymede&amp;#039;s mantle is 1315&amp;amp;nbsp;km thick. Europa&amp;#039;s mantle is 1165&amp;amp;nbsp;km thick.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt; The silicate mantle of the [[Moon]] is approximately 1300–1400&amp;amp;nbsp;km thick.&amp;lt;ref&amp;gt;{{cite journal|last1=Wieczorek|first1=Mark A.|last2=Jolliff|first2=Bradley L.|last3=Khan|first3=Amir|last4=Pritchard|first4=Matthew E.|last5=Weiss|first5=Benjamin P.|last6=Williams|first6=James G.|last7=Hood|first7=Lon L.|last8=Righter|first8=Kevin|last9=Neal|first9=Clive R.|date=2006-01-01|title=The Constitution and Structure of the Lunar Interior|url=https://pubs.geoscienceworld.org/msa/rimg/article-abstract/60/1/221/140775/The-Constitution-and-Structure-of-the-Lunar|journal=Reviews in Mineralogy and Geochemistry|language=en|volume=60|issue=1|pages=221–364|doi=10.2138/rmg.2006.60.3|bibcode=2006RvMG...60..221W|issn=1529-6466}}&amp;lt;/ref&amp;gt; [[Titan (moon)|Titan]] and [[Triton (moon)|Triton]] each have a mantle made of ice or other [[solid]] [[Volatiles|volatile]] [[Substance|substances]].&amp;lt;ref&amp;gt;{{cite web|date=2015-09-14|title=Cassini Solstice Mission: Layers of Titan -- Annotated|url=http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4468|archive-url=https://web.archive.org/web/20150914203834/http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4468|archive-date=2015-09-14|access-date=2020-10-29}}&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;{{cite web|date=2015-11-17|title=Solar System Exploration|url=http://solarsystem.nasa.gov/planets/triton/indepth|archive-url=https://web.archive.org/web/20151117013842/http://solarsystem.nasa.gov/planets/triton/indepth|archive-date=2015-11-17|access-date=2020-10-29}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Asteroids with mantles ==&lt;br /&gt;
Some of the largest [[Asteroid|asteroids]] have mantles.&amp;lt;ref&amp;gt;{{cite web|title=Griffith Observatory - Pieces of the Sky - Meteorite Histories|url=http://www.griffithobservatory.org/exhibits/edgeofspace_piecesofthesky-histories.html|access-date=2020-10-29|website=www.griffithobservatory.org|archive-date=2020-02-10|archive-url=https://web.archive.org/web/20200210150912/http://www.griffithobservatory.org/exhibits/edgeofspace_piecesofthesky-histories.html|url-status=dead}}&amp;lt;/ref&amp;gt; For example, [[Vesta]] has a silicate mantle similar in composition to [[diogenite]] [[meteorites]].&amp;lt;ref&amp;gt;{{cite journal|last1=Reddy|first1=Vishnu|last2=Nathues|first2=Andreas|last3=Gaffey|first3=Michael J.|date=2011|title=First fragment of Asteroid 4 Vesta&amp;#039;s mantle detected|url=https://linkinghub.elsevier.com/retrieve/pii/S0019103510004513|journal=Icarus|language=en|volume=212|issue=1|pages=175–179|doi=10.1016/j.icarus.2010.11.032|bibcode=2011Icar..212..175R}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{Reflist}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Plate tectonics]]&lt;br /&gt;
[[Category:Structure of the Earth]]&lt;/div&gt;</summary>
		<author><name>ImportMaster</name></author>
	</entry>
</feed>