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Konvergerende pladegrænse

Når to tektoniske plader bevæger sig mod hinanden, kaldes det en konvergerende pladegrænse (en subduktionszone). Den tunge oceaniske plade vil i sidste ende synke under den lettere kontinentale plade. Andesbjergene er et eksempel på denne type pladegrænse, den tunge oceaniske plade (Nazca Pladen) bliver trykket ind under den lettere kontinentale Sydamerikanske plade. Læs mere om pladetektonik.

BIllede-kilde: https://arstechnica.com/science/2015/04/magma-beneath-the-cascade-volcanoes-might-be-special-blend/

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