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1 earthquakes recorded in India regional monitoring zone

Real-Time Earthquakes in India

Continuous seismic tracking across the Himalayan Collision Zone, Andaman-Nicobar Subduction Zone, and Peninsular Shield.

INDIA EVENTS

1

TECTONIC SETTING

Indian Plate & Eurasian Plate Continental Collision

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 3.0 13 km NE of Khowai, 26, India

Recent Earthquakes in India

LIVE

Live telemetry feed and seismic report for earthquakes in India.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:HIMALAYAN-FRONTAL-THRUST
Slip Rate:40–50 mm/year convergence
Stress Regime:Continental Collisional Thrusting & Intraplate Compressive Stress

India experiences significant seismic activity driven by the ongoing collision of the Indian Plate with the Eurasian Plate at approximately 40–50 mm/year. This high-stress convergent boundary creates major earthquake risk along the Himalayan Arc, Indo-Gangetic Plains, and Andaman Sea.

Main Himalayan Thrust (MHT / MFT)

Basal Décollement & Thrust

Primary basal detachment underlying the Himalayas capable of producing M8.0+ continental ruptures.

Kutch Mainland Fault (KMF)

Intraplate Reverse Thrust

Active fault in western Gujarat responsible for the destructive 2001 Bhuj earthquake.

Andaman-Nicobar Subduction Zone

Oceanic Subduction Megathrust

Eastern oceanic boundary where the Indian plate subducts beneath the Burma microplate.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2001M 7.7

Bhuj, Kutch, Gujarat

January 26, 2001

Devastating intraplate blind thrust event on Republic Day; destroyed thousands of masonry buildings across Kutch.

2005M 7.6

Kashmir, Western Himalaya

October 8, 2005

Severe thrust faulting along the Balakot-Bagh fault causing catastrophic mountain landslides and structural collapse.

1993M 6.2

Killari / Latur, Maharashtra

September 30, 1993

Intraplate Stable Continental Region (SCR) quake in the Deccan traps that leveled stone-and-mud masonry villages.

Frequently Asked Questions

Common questions about seismic activity, safety, and monitoring in India.

Why do major earthquakes occur in the Himalayas?▾

The Himalayas are formed by the ongoing continental collision between India and Eurasia. The Indian subcontinent continues to push northward at 4 to 5 centimeters per year, accumulating massive elastic strain that releases in major thrust earthquakes.

What are the Seismic Hazard Zones of India?▾

The Bureau of Indian Standards (BIS) categorizes India into four seismic zones: Zone II (Low), Zone III (Moderate), Zone IV (Severe), and Zone V (Very Severe, encompassing the entire Northeast, parts of Jammu & Kashmir, Himachal, Uttarakhand, and Kutch).

How does India monitor tsunami threats?▾

The Indian Tsunami Early Warning Centre (ITEWC) at INCOIS in Hyderabad operates deep ocean DART buoys and coastal tide gauges, issuing warnings within 10 minutes of major subsea earthquakes in the Indian Ocean.