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5th December 2024 (10 Topics)

Telangana (in Safe Seismic Zone) hit by Earthquake

A 5.3-magnitude earthquake jolted Telangana's Mulugu district, with tremors reported in Hyderabad and parts of Andhra Pradesh.

Why it is unusal?

  • Telangana lies in the Indian Peninsular Shield, which is composed of ancient, stable rock formations with minimal tectonic activity compared to plate boundary regions like the Himalayas.
    • Earthquakes in stable regions are typically of low magnitude, and significant quakes are rare.
    • While minor tremors may occur due to localised stress or human-induced activities like mining or reservoir-induced seismicity, the probability of a high-magnitude natural earthquake is extremely low.
  • Telangana rarely experiences seismic activity, making the quake a rare event in the region. Telangana is grouped in Zone II.
    • Zone II typically represents areas with low seismic activity. The average magnitude of earthquakes in such regions depends on the geographical context but generally falls within the magnitude range of 0 to 5.0 on the Richter scale.
  • The quake struck the Mulugu district, with its epicentre near Medaram, which is part of the Godavari rift zone 3.
  • The Godavari rift zone is prone to moderate earthquakes. The recent quake was caused by the release of strain energy along the fault system, occurring at a depth of 40 kilometre.

Seismic zones in India

  • There are four Seismic zones in India: Zone II, Zone III, Zone IV, and Zone V.
  • Zone V expects the highest level of seismicity, whereas Zone II is associated with the lowest level of seismicity.
  • Approximately, 11% of the country falls in zone V, approximately18% in zone IV, approximately 30% in zone III and the remaining in zone II.
  • A total of approximately 59% of the landmass of India (covering all states of India) is prone to earthquakes of different intensities.

Fact Box:

Indian Peninsular Shield 

  • The Peninsular Indian Shield is more than 2,500 million years old, dating back to the Archean Eon. This makes it one of the most ancient geological formations on Earth.
    • A "shield" refers to a large area of exposed Precambrian crystalline igneous and metamorphic rocks that form the stable cores of continents. Shields are characterized by geological stability and resistance to deformation over time.
  • Composition and Structure: The Indian Peninsular Shield consists of an assembly of several Archaean to Early Proterozoic cratons separated by high-grade granulite facies mobile belts. These cratons also serve as the basement to several mid- to late Proterozoic platformal intracratonic basins.
  • Geological Stability: Peninsular India is considered tectonically stable, as it has not been significantly affected by tectonic movements or mountain-building processes in recent geological history. Unlike the Himalayas, which are still undergoing tectonic activity, the Indian Shield has remained largely inactive for millions of years.
  • Composition of Rocks: The Peninsular Indian Shield is primarily composed of ancient igneous and metamorphic rocks, such as granite and gneiss. These are some of the oldest rocks on Earth, providing key insights into the early formation of Earth's crust.
  • Geographical Influence: The stability of the Indian Shield has shaped the geography of Peninsular India. It provides a stable foundation for the land, contributing to the formation of prominent features like the Deccan Plateau, Western Ghats, and Eastern Ghats, which are integral parts of this ancient landmass.

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