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Global Geological And Climatic Events

Taftan Volcano, Iran 

Why in the News?

New satellite data in Geophysical Research Letters (October 2025) shows Iran’s Taftan volcano, dormant for 710,000 years, is reactivating.

Taftan Volcano, Iran 

About Taftan Volcano:

  • Location: Situated in southeastern Iran, about 56 km from the Pakistan border, within the Makran continental volcanic arc.
  • Elevation: Rises to 3,940 metres (12,927 feet), Iran’s only active volcano in the Makran arc.
  • Tectonic Origin: Formed by subduction of the Arabian oceanic plate beneath the Eurasian continental plate.
  • Volcanic Type & Composition: A stratovolcano composed mainly of andesitic and dacitic lava, with pyroclastic flows and volcanic breccias.
  • Structure: Features two summits, Narkuh and Matherkuh, and extensive ignimbrite and lava fans stretching over 30 km.
  • Hydrothermal Activity: Hosts sulfur-emitting fumaroles, visible from up to 100 km, sustained by an active hydrothermal system.
  • Eruptive History: Major activity phases around 8 Ma, 6 Ma, and 0.7 Ma; last lava flow dated to about 6,950 years ago.
  • Recent Observations: 2023–24 satellite data detected 9 cm ground uplift, indicating subsurface pressure buildup and reclassification from extinct to dormant.

Scientific Interpretation and Outlook:

  • Magma Dynamics: Uplift linked to gas accumulation or shallow magma intrusion at 490–630 m depth, possibly fed by deeper chambers (~3.5 km).
  • Current Status: No imminent eruption expected; likely pressure release via degassing or minor eruptions.
  • Monitoring Gap: Lack of ground-based GPS or seismic sensors; reliance on satellite InSAR data for deformation tracking.
  • Scientific Recommendations: Call for establishing a volcano observatory in southeastern Iran for real-time monitoring and gas analysis.
  • Regional Significance: Highlights Makran arc tectonic activity and underscores the need for international geophysical collaboration.
  • Research Importance: Taftan’s reawakening demonstrates the role of remote sensing in detecting hidden volcanic unrest and stresses continuous monitoring to assess eruption potential and regional hazard mitigation.
[UPSC 2024] Consider the following:
1. Pyroclastic debris 2. Ash and dust 3. Nitrogen compounds 4. Sulphur compoundsHow many of the above are products of volcanic eruptions?

Options: (a) Only one (b) Only two (c) Only three (d) only four*

 

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