Wikipedia:Today's featured article/August 12, 2004

From Wikipedia, the free encyclopedia

Plate tectonics is a theory of geology developed to explain the phenomenon of continental drift. In the theory of plate tectonics the outermost part of the Earth's interior is made up of two layers, the outer lithosphere and the inner asthenosphere. Plate tectonic theory arose out of two separate geological observations: seafloor spreading and continental drift. Tectonic plates are broadly divisible into two groups: continental and oceanic plates. The distinction is based on the density of their constituent materials; oceanic plates are denser than continental plates due to their greater mafic mineral content. As a result, the oceanic plates generally lie below sea level, while the continental plates project above sea level.

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