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Earthquake Hazard in Northeast India

Earthquake Hazard in Northeast India

October 7, 2026

Why in News?

A new study assessed earthquake shaking hazard in Northeast India using Probabilistic Seismic Hazard Analysis (PSHA).

Key Facts

Peak Ground Acceleration (PGA) was highest at:

Location PGA
Dibang 0.908 g
Shillong 0.893 g
Guwahati 0.811 g
Itanagar, Imphal, Kohima & Agartala 0.61–0.70 g
Aizawl 0.57 g (comparatively lower)
  • The study used the Das Magnitude Scale instead of the conventional moment magnitude scale.

  • Conventional earthquake magnitude estimates could produce up to 40% higher ground-motion estimates for some medium-sized earthquakes.

Why Are Some Areas More Vulnerable?

Area Cause Effect
Guwahati & Tezpur Soft alluvial deposits of Brahmaputra Basin Ground-motion amplification and liquefaction risk
Shillong Hard Precambrian bedrock and active faults Intense, high-frequency shaking
Kohima & Itanagar – Earthquake shaking and landslide risk
Imphal & Agartala Alluvial/fluvio-lacustrine sediments Basin and site effects
Gangtok & Aizawl Stronger bedrock in many areas; steep slopes Landslide risk

Practice Questions

Prelims Question

Q. Consider the following statements regarding earthquake hazard in Northeast India:

  1. Peak Ground Acceleration was found to be highest near Dibang among the locations studied.

  2. Soft alluvial deposits can amplify earthquake shaking and increase liquefaction risk.

  3. Probabilistic Seismic Hazard Analysis completely eliminates uncertainty arising from limited historical earthquake records.

Which of the statements given above is/are correct?

A. 1 and 2 only
B. 2 and 3 only
C. 1 and 3 only
D. 1, 2 and 3

Answer: A

Explanation: PSHA does not eliminate uncertainty, particularly where earthquake records are limited.

Mains Question

Q. Northeast India is one of India’s most earthquake-prone regions. Discuss the factors responsible for its seismic vulnerability and suggest measures to reduce disaster risk. (150 words)

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