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I am learning about convergent boundaries in the Alipne-Himalaya

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I am learning about convergent boundaries in the Alipne-Himalaya belt. Can an argument be made that the mountain chain is continous form the Alps to the Himalayas? On what basis?

Also How could the Mediterranean have formed? Did the plate boundary types change over time? Could a reversal of plate tectonics have occured, as in the plate margin switching from convergent to divergent?


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