Taftan Volcano Latest News
New research shows that Taftan volcano in Iran seems to be waking up after a 700,000-year-long sleep.
About Taftan Volcano
- It is a 12,927-foot (3,940 meters) semi-active stratovolcano located in southeastern Iran, 56 km from the Pakistan border.
- It is the only active volcano in the Makran continental volcanic arc.
- It is situated among a rumple of mountains and volcanoes that was formed by the subduction of the Arabian ocean crust under the Eurasian continent.Â
- It hosts an active hydrothermal system and smelly, sulfur-emitting vents called fumaroles.
- The volcano contains two summits (Narkuh and Matherkuh).
- It isn't known to have erupted in human history.
What is a Stratovolcano?
- It is a tall, steep, and cone-shaped type of volcano.
- Unlike flat shield volcanoes, they have higher peaks.
- They are typically found above subduction zones, and they are often part of large volcanically active regions, such as the Ring of Fire that frames much of the Pacific Ocean.
- Stratovolcanoes comprise the largest percentage (~60%) of the Earth’s individual volcanoes, and most are characterized by eruptions of andesite and dacite, lavas that are cooler and more viscous than basalt.
- These more viscous lavas allow gas pressures to build up to high levels. Therefore, these volcanoes often suffer explosive eruptions.Â
- They are usually about half-half lava and pyroclastic material, and the layering of these products gives them their other common name of composite volcanoes.
- At the peak, stratovolcanoes usually have a small crater.
Source: LS
Taftan Volcano FAQs
Q1: Where is the Taftan Volcano located?
Ans: Southeastern Iran
Q2: What type of volcano is the Taftan Volcano?
Ans: Stratovolcano
Q3: What is the approximate height of the Taftan Volcano?
Ans: 3,940 meters
Q4: What geological process led to the formation of the Taftan Volcano?
Ans: Subduction of the Arabian ocean crust under the Eurasian continent.