Recently, a 7.7-magnitude earthquake struck Myanmar causing severe damage in Mandalay and affecting neighboring countries.
About the Myanmar Earthquake

- The Myanmar Earthquake is the strongest globally in two years, and was followed by multiple aftershocks.
- Parts of Northeast India also felt tremors, but no major casualties or damage were reported.
- The epicenter was 17.2 km from Mandalay, at a shallow depth of 10 km, intensifying the damage.
- The shallow depth (10 km) of the recent earthquake intensified its ground shaking, leading to widespread destruction.
- Shallower earthquakes cause greater surface damage compared to deeper ones.
Impact of the Earthquake
- The U.S. Geological Survey (USGS) Earthquake Hazards Program estimated potential fatalities between 10,000 and 100,000.
- Economic losses up to 70% of Myanmar’s GDP.
- The central region of Myanmar, where the recent quake struck, is less accustomed to large earthquakes, worsening the impact.
Frequency of Earthquakes in Myanmar
- Myanmar has experienced at least six earthquakes above magnitude 7 since 1900.
- Notable earthquakes:
- 1990 (Magnitude 7.0): 32 buildings collapsed.
- 1912 (Magnitude 7.9): Near the recent earthquake’s epicenter.
- 2016 (Magnitude 6.9): Affected the same region.
- Over the last 100 years, Myanmar has recorded 14 earthquakes of magnitude 6 or above.
- The 1839 earthquake (Magnitude 8.3) was one of the most destructive, killing 300-400 people.
Earthquake due to tectonic activity
- The Earth’s lithosphere consists of moving tectonic plates, interacting over billions of years.
- Earthquakes occur when plates slip past each other, releasing stored seismic energy.
Factors Responsible for Frequent Earthquakes in Myanmar
- Myanmar’s location between two tectonic plates : The location between the India and Eurasia plates places it at particular risk of earthquakes.
- The boundary between the two plates is called the Sagaing Fault
- Myanmar’s Sagaing Fault is a major north-south fault line, highly prone to seismic activity.
- It marks the tectonic boundary between the Indian Plate (moving north) and the Eurasian Plate.
-
- The recent earthquake was caused by strike-slip faulting, where the plates move sideways against each other.
- Earthquakes affect regions beyond the epicenter due to seismic waves spreading along the fault line.
India’s Response to the Myanmar Earthquake
- Operation Brahma : India delivered 15 tonnes of relief materials to Myanmar using a C-130J military transport aircraft of the Indian Air Force under operation Brahma.
- Rescue Support: India deployed 80 National Disaster Response Force (NDRF) personnel to assist in rescue and relief operations in quake-hit areas.
- Humanitarian Assistance: Alongside China and Russia, India extended immediate aid, reaffirming its commitment to regional disaster response and support.
Additional Reading: Earthquakes
To get PDF version, Please click on "Print PDF" button.