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What is an orogenic belt?

An orogenic belt, also called an orogen or mobile belt, is a region of Earth's crust that has been deformed and uplifted to form mountain ranges through a process known as orogenesis. These zones typically develop when continental plates crumple together or when oceanic plates and crustal fragments accrete over vast geological timescales. Major examples include the Central Asian Orogenic Belt and the vast Alpide belt stretching across Eurasia.

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