The Taftan Volcano in Iran is showing signs of reawakening after 700,000 years. It is a 12,927-foot or 3,940-metre-high semi-active stratovolcano. It lies in southeastern Iran, about 56 kilometres from the Pakistan border. It is the only active volcano in the Makran continental volcanic arc. The volcano formed due to the subduction of the Arabian Ocean crust beneath the Eurasian continent. It has two summits named Narkuh and Matherkuh. Taftan has an active hydrothermal system with sulfur-emitting vents called fumaroles. It has not erupted in recorded human history.
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