Geography and Environment
The Taftan Volcano in southeastern Iran has shown signs of renewed activity after nearly 700,000 years of dormancy. Scientists have observed increased geothermal emissions and seismic tremors, indicating possible reactivation within this long-inactive volcanic system.
This development holds significant geological and regional importance. It provides rare evidence of volcanic reawakening in the Makran arc, a tectonically active region better known for subduction-related earthquakes. While the increased geothermal activity may pose potential risks to nearby settlements and infrastructure, it also presents opportunities for harnessing geothermal energy.
Scientifically, Taftan’s reactivation enhances understanding of the Arabian–Eurasian plate interaction and contributes to broader research on seismic and volcanic hazards in Iran, Pakistan, and Afghanistan.
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