マントル対流説
1. Mantle convectionMantle convection is the slow creeping motion of Earth's rocky 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.
Read “Mantle convection” on English Wikipedia
Read “マントル対流説” on Japanese Wikipedia
Read “Mantle convection” on DBpedia
Read “Mantle convection” on English Wikipedia
Read “マントル対流説” on Japanese Wikipedia
Read “Mantle convection” on DBpedia
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