Dosyeya orjînal(880 × 600 pixel, mezinbûnê data: 65 KB, MIME-typ: image/png)


Danasîn

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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Derivative works of this file:  Destructive plate margin.svg

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Dîroka daneyê

Ji bo dîtina guhartoya wê demê bişkoka dîrokê bitikîne.

Dîrok/KatjimêrWêneyê biçûkMezinahîBikarhênerŞirove
niha17:35, 4 kanûna pêşîn 2004Versiyona biçûkkirî yê 17:35, 4 kanûna pêşîn 2004880 x 600 (65 KB)Ævar Arnfjörð Bjarmason

Ev rûpelên li jêr vê dosyeyê bi kar tînin:

Bikaranîna gerdûnî ya pelê

Ev wîkiyên di rêzê de vê pelê bi kar tînin:

Zêdetir bikaranîna global a vê pelê bibîne.