Fukutoku-Okanoba Volcano

Fukutoku-Okanoba Volcano is an active submarine volcano that is part of the Volcano Islands of Japan in the Pacific Ocean. Read more about Fukutoku-Okanoba Volcano, Location, Eruption, Latest News.

Fukutoku-Okanoba Volcano
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Fukutoku-Okanoba Volcano Latest News

Japan’s Coast Guard recently reported signs of activity at the Fukutoku-Okanoba submarine volcano. 

About Fukutoku-Okanoba Volcano

  • It is an active submarine volcano that is part of the Volcano Islands of Japan in the Pacific Ocean.  
  • It is part of the Izu-Bonin arc formed by subduction of the Pacific Plate beneath the Philippine Sea Plate. 
  • Its summit is just 14 meters (46 feet) below sea level, allowing Surtseyan eruptions to breach the surface.  
  • Composition is tholeiitic basalt, typical of arc front volcanism. 
  • It remains active with intermittent submarine eruptions and discoloured water since 2013. 
  • Eruptions are explosive with pumice rafts, discoloured water, and occasional ephemeral island formation. 
  • The 2021 eruption produced massive pumice rafts that drifted thousands of kilometres across the Pacific, impacting shipping and beaches. 
  • The volcano’s frequent activity and shallow depth make it one of the most dynamic submarines, with eruptions often detected by satellite discoloration.  

What is a Surtseyan Eruption?

  • It is a type of volcanic eruption that takes place in shallow seas or lakes. 
  • It is named after the island of Surtsey off the southern coast of Iceland. 
  • When magma rises close to the surface of the water, it can come into contact with the water and cause it to flash to steam. 
  • The sudden increase in volume of the steam can cause an explosion, which can fragment the magma into small pieces. 
  • These pieces of magma, called tephra, can be ejected into the air, forming an ash column. 
  • These eruptions are commonly phreatomagmatic eruptions, representing violent explosions caused by rising basaltic or andesitic magma coming into contact with abundant, shallow groundwater or surface water. 
  • Tuff rings, pyroclastic cones of primarily ash, are built by explosive disruption of rapidly cooled magma.
  • Surtseyan eruptions are relatively common, and they can be found all over the world.  
  • Surtseyan eruptions can be very dangerous. 
    • The ash and rock fragments that are ejected into the air can travel long distances, and they can be a hazard to ships and aircraft. 
    • The sudden expansion of steam can also cause shock waves, which can damage buildings and other structures.

News: REUT

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Fukutoku-Okanoba Volcano FAQs

Q1. What is Fukutoku-Okanoba?+

Q2. Which volcanic arc is Fukutoku-Okanoba part of?+

Q3. What type of eruptions can occur at Fukutoku-Okanoba due to its shallow depth?+

Q4. What is the composition of Fukutoku-Okanoba Volcano?+

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