About: dbpedia:Mantle

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Mantle convection is the slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior of the Earth to the surface. The Earth's surface lithosphere, which rides atop the asthenosphere (the two components of the upper mantle), is divided into a number of plates that are continuously being created and consumed at their opposite plate boundaries.

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rdfs:comment	Mantle convection is the slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior of the Earth to the surface. The Earth's surface lithosphere, which rides atop the asthenosphere (the two components of the upper mantle), is divided into a number of plates that are continuously being created and consumed at their opposite plate boundaries.
rdfs:seeAlso	dbpedia:Heat_transfer
foaf:depiction
thumbnail	http://commons.wikimedia.org/wiki/Special:FilePath/Earth-crust-cutaway-numbered.svg?width=300

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