Global Geological And Climatic Events

Massive Earthquake hits Myanmar and Thailand

Note4Students

From UPSC perspective, the following things are important :

Prelims level: Earthquakes

Why in the News?

A powerful 7.7 magnitude earthquake struck Myanmar, with its epicentre near Mandalay, the country’s second-largest city.

Massive Earthquake hits Myanmar and Thailand

What caused the Earthquake in Myanmar?

  • Myanmar is situated between the Indian Plate and the Eurasian Plate, which makes the region seismically active.
    • The Sagaing Fault, running from north to south through Myanmar, marks the boundary of these plates.
    • It is an active fault line that has caused significant earthquakes in the past, including a 7.9 magnitude earthquake in 1912 and a 6.9 magnitude earthquake in 2016.
  • The Indian Plate was moving northward along the Sagaing Fault relative to the Eurasian Plate.
    • The friction and stress built up along this fault led to a sudden release of energy, resulting in the earthquake.
  • The earthquake’s epicentres was located 17.2 km from Mandalay, Myanmar’s second-largest city, at a depth of just 10 km.

Why are Shallow Earthquakes more destructive?

  • Proximity to the Surface: Shallow earthquakes (less than 70 km deep) cause intense shaking. For example, the Myanmar earthquake occurred at 10 km, leading to rapid, forceful seismic waves and extensive damage.
  • Energy Release: Shallow earthquakes retain more energy in seismic waves, causing stronger surface shaking and greater destruction.
  • Higher Intensity: Shallow quakes produce higher intensity shaking, resulting in more structural damage compared to deeper quakes, where seismic waves lose energy.
  • Aftershocks: Shallow earthquakes often lead to more intense aftershocks, further damaging already weakened structures. The Myanmar earthquake had aftershocks, including one with magnitude 6.4.

Back2Basics: Earthquake and Related Terminologies

  • Earthquake is a sudden shaking of the ground caused by energy release from tectonic plate movements or volcanic activity, generating seismic waves.
  • Key Terminologies:
    • Focus (Hypocenter): The point inside the Earth where the earthquake originates, deep beneath the surface.
    • Epicenter: The point on the Earth’s surface directly above the focus, usually the most affected area.
    • Seismic Waves: Waves that carry the energy released during an earthquake and cause ground shaking.
    • Fault: A crack or fracture in the Earth’s crust where movement occurs, often causing earthquakes.
    • Magnitude: A measure of the earthquake’s size or energy, commonly measured on the Richter scale.
    • Intensity: The strength of shaking at specific locations, measured by the Modified Mercalli Intensity (MMI) scale.

Types of Earthquake Waves:

  • Body Waves: Travel through the Earth’s interior, detected first by seismographs.
    • Primary Waves (P-Waves): Fastest, compression waves that move through solids and liquids.
    • Secondary Waves (S-Waves): Shear waves, slower than P-waves, that move through solids only.
  • Surface Waves: Travel along the Earth’s surface, slower but cause more damage.
    • Love Waves: Move side-to-side horizontally, causing significant damage.
    • Rayleigh Waves: Cause elliptical ground motion, similar to ocean waves, very destructive.

 

[UPSC 2021] Consider the following statements:

1. In a seismograph, P waves are recorded earlier than S waves.

2. In P waves, the individual particles vibrate to and fro in the direction of waves propagation whereas in S waves, the particles vibrate up and down at right angles to the direction of wave propagation.

Which of the statements given above is/are correct?

(a) 1 only (b) 2 only (c) Both 1 and 2 (d) Neither 1 nor 2

 

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