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Earthquakes

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February 18, 2025

Why in News?

Recently the National Capital Region, Delhi and adjoining regions faces a shallow earthquake of 4.0 magnitude with a focal depth of five kilometres.

  • An earthquake is a phenomenon that occurs without warning and involves violent shaking of the ground and everything over it.
  • It results from the release of accumulated stress of the moving lithospheric or crustal plates.
  • An earthquake is the sudden movement of Earth’s crust at a fault line.
  • It is also called as quakes, tremors, or temblors.
  • Epicenter - The location where an earthquake begins is called the epicenter. An earthquake’s most intense shaking is often felt near the epicenter.
  • However, the vibrations from an earthquake can still be felt and detected hundreds, or even thousands of miles away from the epicenter.
  • The energy from an earthquake travels through Earth in vibrations called seismic waves, measured by seismometer.
  • Types of energy

P waves or primary waves

  • These are the first waves to be detected.
  • These are compressional waves that push and pull as they move through rock and fluids.

S waves or secondary waves

  • These are the second waves to be detected.
  • These waves move only through rock.
  • They move up and down or side to side, perpendicular to the direction in which the wave is moving.

Surface waves

  • It follows P and S waves.
  • They travel along the surface of the earth and thus cause the most damage.
  • Surface waves can be characterized as Love waves, which are faster and move the ground from side to side.
  • Types Of Earthquake - Along with the tectonic earthquakes, there are also 3 types of earthquakes.
    • Volcanic - Earthquakes that occur in conjunction with volcanic activity
    • Collapse - Smaller-scale earthquakes that result from the subterranean collapse of caverns or mines
    • Explosion - Earthquakes caused by underground explosions of nuclear or chemical devices.
  • Depth
    • Shallow earthquakes - 0 to 70 km deep
    • Intermediate earthquakes - 70 to 300 km deep.
    • Deep earthquakes - 300 to 700 km deep.
  • Scenario in Delhi - Delhi lies in the Aravalli-Delhi Fold Belt, a seismically-active geological belt extending from southern and eastern Rajasthan to Haryana and Delhi.
  • Over the years, the tectonic activity in the region has slowed down considerably, leading to greater geological stability. But some faults still remain, which give rise to occasional mild earthquakes.
  • Medvedev-Sponheuer-Karnik scale – It is a measure of intensity, rather than strength, or energy released, which is described by magnitude.
  • Delhi is classified in Zone 4, the 2nd highest classification of areas based on their susceptibility to shaking experienced during an earthquake.

References

  1. The Hindu | What is a shallow earthquake?
  2. News 18 | What Is an Earthquake?
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