Mynd:Destructive_plate_margin.png
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Lýsing
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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This work has been released into the public domain by its author, Fredrik at enska Wikipedia. This applies worldwide. In some countries this may not be legally possible; if so: Fredrik grants anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law.Public domainPublic domainfalsefalse |
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Dagsetning/Tími | Smámynd | Víddir | Notandi | Athugasemd | |
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núverandi | 4. desember 2004 kl. 17:35 | 880 × 600 (65 KB) | Ævar Arnfjörð Bjarmason |
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