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The Earth and Planetary Sciences
George W. Wetherill and Charles L. Drake
New Series, Vol. 209, No. 4452, Centennial Issue (Jul. 4, 1980), pp. 96-104
Published by: American Association for the Advancement of Science
Stable URL: http://www.jstor.org/stable/1684842
Page Count: 9
You can always find the topics here!Topics: Earth, Plate tectonics, Oceans, Rocks, Continents, Lithospheres, Geology, Mantle, Terrestrial planets, Venus
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During the last two decades the earth sciences community has become persuaded that the earth is a dynamic body; an engine driven by its internal heat. The major surface manifestation of this dynamism has been fragmentation of the earth's outer shell and subsequent relative horizontal movement of the pieces on a large scale. The driving force is convection within the earth, but much remains to be learned about the nature of the convection and the composition of the earth's interior. The other terrestrial planets show evidence of once having been hot, but their surfaces suggest long-term stability and lack evidence of continuing convection.
Science © 1980 American Association for the Advancement of Science