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Iran features fold mountains primarily due to the collision of tectonic plates, specifically the Arabian and Eurasian plates, which create significant geological uplift and deformation. This process results in the formation of mountain ranges like the Zagros. However, the lack of active volcanic activity in Iran is attributed to the nature of these tectonic interactions, which predominantly involve compressional forces rather than subduction processes that typically generate volcanoes. Thus, while Iran has impressive fold mountains, it does not have the volcanic activity commonly associated with subduction zones.

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20h ago

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