File:Destructive plate margin.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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Category:Diagrams of oceanic trenches Category:Volcanological diagrams Category:Language-neutral geological diagrams Category:Media missing infobox template
Category:Diagrams of oceanic trenches Category:Files with derivative versions Category:Files with no machine-readable author Category:Files with no machine-readable source Category:Language-neutral geological diagrams Category:Media missing infobox template Category:PD-user Category:Vector version available Category:Volcanological diagrams