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Q25. Discuss the geophysical characteristics of Circum- Pacific Zone.

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Introduction
The Circum-Pacific Belt, also referred to as The Ring of Fire, is a path along the Pacific Ocean characterized by active volcanoes and frequent earthquakes.

Body

  • Location: A nearly continuous chain of volcanoes surrounds the Pacific Ocean. The chain passes along the west coast of North and South America, from the Aleutian Islands to the south of Japan, from Indonesia to the Tonga Islands, and New Zealand.
  • Formation: This Circum-Pacific chain of volcanoes (often called the Ring of Fire) and the mountain ranges associated with it owe their formation to the repeated subduction of the oceanic lithosphere beneath the continents and the islands that surround the Pacific Ocean.
    • The Ring of Fire is the result of plate tectonics (Convergent, Divergent Plate Boundary, Transform Plate Boundary).
  • Harbors Majority of Volcano & Earthquakes: Seventy-five percent of Earth’s volcanoes—more than 450 volcanoes—are located along the Ring of Fire.
    • Ninety percent of Earth’s earthquakes occur along its path, including the planet’s most violent and dramatic seismic events.
  • List of Some Volcano Circum-Pacific Belt: Mount Fuji of Japan, The Aleutian Islands of US, Krakatau Island Volcano in Indonesia, etc.
  • Formation of Hot Spots: The Ring of Fire is also home to hot spots, areas deep within the Earth’s mantle from which heat rises.
    • This heat facilitates the melting of rock in the brittle, upper portion of the mantle. The melted rock, known as magma, often pushes through cracks in the crust to form volcanoes.

Conclusion
As the Circum-Pacific Belt harbors the majority of global Volcanic eruptions & Earthquakes, it holds immense significance regarding the study of the earth’s interior.

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FAQs on GS1 PYQ (Mains Answer Writing): Circum-Pacific Zone - UPSC Mains Answer Writing: Practice

1. What is the Circum-Pacific Zone?
Ans. The Circum-Pacific Zone, also known as the Ring of Fire, is a region around the edges of the Pacific Ocean where a large number of earthquakes and volcanic eruptions occur. It is characterized by intense seismic activity and is home to about 75% of the world's active volcanoes.
2. What are the major tectonic plates involved in the Circum-Pacific Zone?
Ans. The Circum-Pacific Zone is formed by the interaction of several tectonic plates, including the Pacific Plate, the North American Plate, the Philippine Sea Plate, the Juan de Fuca Plate, and the Cocos Plate. These plates are constantly moving and interacting, leading to the formation of earthquakes and volcanic activity in the region.
3. How does the Circum-Pacific Zone affect earthquake and volcanic activity?
Ans. The Circum-Pacific Zone is a highly active seismic region due to the subduction of tectonic plates. Subduction occurs when one tectonic plate is forced beneath another, leading to the formation of deep ocean trenches and volcanic arcs. This process results in the release of energy in the form of earthquakes and volcanic eruptions.
4. What are the potential hazards associated with the Circum-Pacific Zone?
Ans. The Circum-Pacific Zone is prone to several hazards, including earthquakes, tsunamis, and volcanic eruptions. These events can cause widespread damage to infrastructure, loss of life, and economic disruptions. The region is also at risk of secondary hazards such as landslides and avalanches triggered by seismic activity.
5. How does the Circum-Pacific Zone impact the countries located within its boundaries?
Ans. The countries located within the Circum-Pacific Zone, such as Japan, Indonesia, and the Philippines, are particularly vulnerable to the hazards associated with this region. These countries have implemented various measures to mitigate the risks, including early warning systems for earthquakes and tsunamis, building codes for earthquake-resistant structures, and evacuation plans for volcanic eruptions. However, the frequency and intensity of natural disasters in the region continue to pose challenges for these countries.
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