Dosya:Destructive plate margin.png

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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.

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Image by Fredrik.

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Public domain Na karkerdış heta nuskar de Fredrik at English Wikipediya ra biya malê şari deye hesereyaya. Dınya heme ca dı ravêrena.
Tay dewletan dı no kanuniyey heta mıkum nêbone; o haldı:
Ez, ena Fredrik qande herhangi yew amaci, be şert, hendı ke legali icab nikeni, şari hemi re ezo mısade dana.

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Tarix/ZemanResımo qıckekEbadiKarberMışewre
nıkayên17:35, 4 Kanun 2004Seba versiyonê 17:35, 4 Kanun 2004 ra880 - 600 (65 KB)Ævar Arnfjörð Bjarmason

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