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Rozbieżna granica płyt tektonicznych

Jest to typ granicy, w której płyta jest rozsuwana na dwie oddzielne płyty. W efekcie pomiędzy płytami powstaje nowa skorupa. Przykładem takiej granicy jest grzbiet środkowoatlantycki.

Źródło: https://scullyproject.wikispaces.com/Divergent+Boundary+(Pictures)

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