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File:Destructive plate margin.png

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to rise. The magma rises up through weak areas in the continental crust, eventually erupting as one or more
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causes the oceanic crust to evaporate, and reduced density forces the newly formed
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File:Destructive plate margin.png
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Destructive plate margin
Friction
earthquakes
asthenosphere
magma
volcanoes
Fredrik

File:Destructive plate margin.svg
File:Destructive plate margin.svg
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