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File:Destructive plate margin.png

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Original file ‎(880 × 600 pixels, file size: 65 KB, MIME type: image/png)

Summary

Destructive plate margin; oceanic crust is forced below the continental crust because oceanic crust is denser than continental crust. Friction between the moving plates causes earthquakes. The heat increase due to friction and being pushed into the asthenosphere causes the oceanic crust to evaporate, and reduced density forces the newly formed magma to rise. The magma rises up through weak areas in the continental crust, eventually erupting as one or more volcanoes.

Not to scale.

Image by Fredrik.

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current17:35, 4 December 2004Thumbnail for version as of 17:35, 4 December 2004880 × 600 (65 KB)Ævar Arnfjörð Bjarmason
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