Day 39 – Q. 1. Why is the Circum-Pacific Belt known as the most active seismic and volcanic region in the world? Discuss the tectonic settings responsible for this activity. (150 words, 10 marks)

  • IASbaba
  • July 16, 2025
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Ethics Theory, TLP-UPSC Mains Answer Writing

Q. 1. Why is the Circum-Pacific Belt known as the most active seismic and volcanic region in the world? Discuss the tectonic settings responsible for this activity. (150 words, 10 marks)


Introduction 

The Circum-Pacific Belt, also known as the “Ring of Fire”, encircles the Pacific Ocean and  accounts for over 75% of the world’s active volcanoes and 90% of earthquakes, due to its  complex tectonic environment. 

Body

Reasons for high seismic and volcanic activity 

  1. Subduction of oceanic plates: The  Pacific Plate and other oceanic  plates are subducting beneath  continental plates, leading to intense earthquake and volcanic  activity.
  2. Presence of multiple convergent  boundaries: Regions like the Andes,  Japan, and Indonesia experience  frequent seismicity due to constant  plate collision.
  3. Accumulated strain and sudden  release: The constant movement  leads to stress accumulation in  rocks, resulting in sudden energy  release during earthquakes.
  4. Formation of island arcs and trenches: Features like the Mariana Trench and Aleutian  Islands are direct results of subduction processes that foster both volcanism and  seismicity. 

Tectonic settings responsible 

  1. Oceanic-continental subduction zones: Nazca Plate subducting beneath South America  forms the Andes and triggers frequent earthquakes. 
  2. Oceanic-oceanic subduction zones: The Pacific Plate subducting under the Philippine Sea  Plate forms deep-sea trenches and island arcs. 
  3. Transform fault boundaries: The San Andreas Fault in California causes lateral movement  and frequent shallow earthquakes. 
  4. Multiple plate junctions: Regions like Japan lie at the intersection of four tectonic plates,  increasing seismic complexity. 
  5. Ring-shaped tectonic convergence: The continuous loop of interacting plates around the  Pacific leads to persistent and intense geodynamic activity. 

Conclusion

The Circum-Pacific Belt exemplifies how tectonic interactions—especially subduction and  transform boundaries—create a dynamic geological zone. Understanding its structure helps  mitigate disaster risk through better prediction and resilient infrastructure in vulnerable  regions.

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