Iran’s Taftan Volcano. Source: Discover (image by Tripper92/Shutterstock)
The Taftan Volcano in southeastern Iran, long thought to be extinct, is showing signs of renewed activity after approximately 700,000 years of dormancy. Recent satellite data analyzed between July 2023 and May 2024 revealed a ground uplift of around 9 centimeters, indicating an increase in pressure beneath the summit. This gradual rise has not receded, suggesting a sustained buildup of gas or fluid within the volcano’s subsurface system.
Located near the border with Pakistan, Taftan is a 3,940-meter stratovolcano formed by the subduction of the Arabian Plate beneath the Eurasian Plate. Although no eruptions have occurred in recorded history, fumarolic emissions and sulfur vents have been active in recent years, with residents from the nearby city of Khash reporting strong sulfuric odors in 2023. The findings, published in Geophysical Research Letters, confirm that Taftan is not extinct but rather dormant and potentially active.
Using data from the European Space Agency’s Sentinel-1 mission, researchers employed Interferometric Synthetic Aperture Radar (InSAR) to detect subtle surface movements with high precision. The uplift’s source was estimated to lie between 490 and 630 meters below the surface, at a shallow depth relative to the deeper magma reservoir situated roughly 3.5 kilometers down.
Displacement velocity (Line of Sight) in the Taftan region, processed using SNAP and StaMPS software. Source: IPRS Annals of the Photogrammetry
Scientists ruled out external triggers such as heavy rainfall or nearby seismic activity. The most probable explanations include a build-up of volcanic gases or a small influx of magma causing rock pore pressure to rise and the ground to deform upward. Though this deformation does not indicate an imminent eruption, it underscores the need for closer gas monitoring and seismic observation in the region.
Researchers emphasize that this phenomenon is not a cause for alarm but a scientific warning to establish regular monitoring programs. Taftan’s current state provides valuable insight into early volcanic reactivation processes and the interactions between hydrothermal systems and shallow magma activity. Understanding the volcano’s behavior is vital for assessing potential hazards to surrounding communities and for improving volcano monitoring strategies in tectonically active but under-instrumented regions like southeastern Iran.
Geoengineer.org uses third party cookies to improve our website and your experience when using it. To find out more about the cookies we use and how to delete them visit our Cookies page. Allow cookies