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Earthquakes

29-03-2025

06:28 AM

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1 min read
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A 7.7-magnitude earthquake struck central Myanmar on March 29, 2025, causing significant destruction in Mandalay and claiming at least 144 lives.

About Earthquakes

  • Earthquake: Sudden shaking or trembling of the Earth's surface due to the release of stored energy in the Earth's crust or upper mantle.
  • Focus (Hypocentre): The point within the Earth where the earthquake originates.
  • Epicentre: The point on the surface directly above the focus.
  • Seismograph: An instrument used to detect and measure earthquakes.
  • Isoseismic line: A line connecting points on the surface experiencing the same intensity.

Types of Seismic Waves

Type

Description

Speed

Primary (P) Waves

Fastest, travel through solids, liquids, and gases

Fastest

Secondary (S) Waves

Travel through solids only, cause more damage

Slower than P-waves

Surface Waves

Slowest, cause maximum destruction

Slowest

Causes of Earthquakes

  • Fault zones: Most earthquakes occur along fault lines, where stress builds up due to tectonic movements.
  • Major faults:
    • Thrust faults (Convergent boundary) → Most powerful quakes (Magnitude 8+).
    • Strike-slip faults (Transform boundary) → Horizontal movement (e.g., Sagaing Fault, San Andreas Fault).
    • Normal faults (Divergent boundary) → Less intense quakes (Magnitude <7).
  • Plate Tectonics: Tectonic movement at plate boundaries can trigger earthquakes:
    • Convergent BoundariesSubduction zones, causing megathrust earthquakes (e.g., 2004 Indian Ocean earthquake).
    • Divergent BoundariesSpreading ridges generate mild earthquakes.
    • Transform BoundariesHorizontal movement of plates leads to strike-slip earthquakes (e.g., Sagaing Fault, San Andreas Fault).
  • Volcanic activity: Magma movement inside volcanoes can cause volcanic earthquakes.
    • Myanmar has active volcanoes, contributing to seismic activity.
  • Human-induced earthquakes: Mining, dam construction, and deep drilling can trigger artificial seismic activity.

Why Does Myanmar Experience Frequent Earthquakes?

  • Tectonic Setting: Myanmar lies at the junction of three major tectonic plates:
    • Indian Plate (moving northward)
    • Eurasian Plate (moving southward)
    • Burma Microplate (moving eastward)
  • The Sagaing Fault, a strike-slip fault, runs north-south through central Myanmar, making it highly prone to seismic activity.

Earthquakes FAQs

Q1. What causes earthquakes?
Ans. Earthquakes are caused by the sudden release of energy due to the movement of tectonic plates along faults.

Q2. What is the difference between the Richter scale and the Mercalli scale?
Ans. The Richter scale measures earthquake magnitude (energy released), while the Mercalli scale measures the intensity and impact on people and structures.

Q3. What are the major earthquake-prone zones in India?
Ans. India has four seismic zones. Zone V (most active) includes regions like the Himalayas and the Northeast, while Zone II (least active) includes central and southern India.

Q4. What is the significance of the Ring of Fire in earthquakes?
Ans. The Ring of Fire is a highly seismically active zone in the Pacific Ocean where most of the world's earthquakes and volcanic eruptions occur due to subduction zones.

Q5. What are the mitigation strategies for earthquakes?
Ans. Earthquake mitigation includes retrofitting buildings, enforcing seismic-resistant construction codes, early warning systems, and public awareness programs.

Source: IE