Myanmar Earthquake: Why It’s So Powerful and Damaging
- BANGKOK (AP) — The death toll from a powerful magnitude 7.7 earthquake in Myanmar has risen to over 1,000, officials said Saturday.
- The earthquake's epicenter was located in the Sagaing region, near Mandalay, at a shallow depth of 10 kilometers along the Sagaing fault, a horizontal strike-slip fault.
- State-run television MRTV reported that 694 people had been confirmed dead as of Saturday, with another 1,670 injured, according to a statement from the military-led government.
Myanmar Earthquake death Toll Jumps to Over 1,000
Table of Contents
- Myanmar Earthquake death Toll Jumps to Over 1,000
- Myanmar Earthquake: what You Need to no
- How Many People Died in the Myanmar Earthquake?
- What Caused the Myanmar Earthquake?
- Where Did the Earthquake Occur?
- How Strong Was the myanmar Earthquake?
- What Areas Were Affected by the Earthquake?
- Why Was the Earthquake So Destructive?
- What Type of Fault Caused the Earthquake?
- Is Myanmar Prone to Earthquakes?
- How Does the Earthquake Compare to Previous Events?
- What’s the Impact on infrastructure?
- Key Facts and Figures in Summary:
BANGKOK (AP) — The death toll from a powerful magnitude 7.7 earthquake in Myanmar has risen to over 1,000, officials said Saturday. The quake, wich struck Friday, caused widespread damage.
The earthquake’s epicenter was located in the Sagaing region, near Mandalay, at a shallow depth of 10 kilometers along the Sagaing fault, a horizontal strike-slip fault.
State-run television MRTV reported that 694 people had been confirmed dead as of Saturday, with another 1,670 injured, according to a statement from the military-led government. However, by Saturday, the death toll had surpassed 1,000 as more bodies were recovered from the rubble.
Neighboring countries,including Thailand and China,also felt the effects of the quake. In Bangkok, Thailand, there were reports of 10 fatalities and several collapsed buildings.
The earthquake is considered the largest to strike Myanmar since 1912 and the deadliest and most destructive since the contry’s independence in 1948.
Seismic Activity in Myanmar
Myanmar is situated on the border between two tectonic plates, making it one of the world’s most seismically active regions. While large, destructive earthquakes are relatively rare in the Sagaing region, the country is vulnerable.
Joanna Faure Walker, a professor and earthquake expert at University College London, explained, The limit of the plate between the Indian plate and the Eurasian plate stretches from north to south, dividing the middle of the country.
Walker noted that the plates move past each other horizontally at varying speeds. While this type of movement causes strike-slip
earthquakes, which are generally not as strong as those occurring in subduction zones, they can still reach magnitudes of 7 to 8.
The Sagaing region has experienced several earthquakes in recent years, including a magnitude 6.8 quake in 2012 that killed at least 26 people and injured dozens more.
Bill McGuire, an earthquake expert at UCL, described the March 28, 2025, earthquake as perhaps the largest
to hit Myanmar in the last 75 years.
Shallow Depth Intensifies Damage
The shallow depth of the earthquake, less than 70 kilometers from the surface, amplified its destructive impact. Roger Musson, a researcher at the British geological Survey, explained that this shallow depth meant that the shock wave does not disappear when moving from the epicenter to the surface. Buildings receive full strength from shocks.
Musson emphasized that it is indeed crucial to consider the entire fault line rather than focusing solely on the epicenter,as seismic waves spread from the entire fault.
Regarding predictions that the earthquake’s fatalities could reach 10,000 and shake 7% of Myanmar’s GDP, Musson stated that these estimates were based on data from previous earthquakes, the overall size and location of the event, and Myanmar’s preparedness for earthquakes.
The infrequency of large seismic events in the Sagaing region suggests that infrastructure may not have been built to withstand strong shocks, potentially exacerbating the damage. Musson noted that the last major earthquake in the region occurred in 1956, meaning that many buildings were not constructed to withstand Friday’s seismic forces.
Most of the earthquake in Myanmar occurred in the western region, while this earthquake occurred in the central region of the country,
Musson said.
Myanmar Earthquake: what You Need to no
Understanding the devastation
How Many People Died in the Myanmar Earthquake?
The death toll from the powerful magnitude 7.7 earthquake in Myanmar has tragically surpassed 1,000, as of March 29, 2025. This figure is based on the recovery of bodies from the rubble. This makes it the deadliest and most destructive as Myanmar’s independence in 1948.
What Caused the Myanmar Earthquake?
The earthquake originated in the Sagaing region, near Mandalay, Myanmar. It was caused by movement along the Sagaing fault, a horizontal strike-slip fault. This type of fault occurs when tectonic plates slide past each other.
Where Did the Earthquake Occur?
The epicenter of the earthquake was located in the Sagaing region of Myanmar, close to the city of Mandalay.
How Strong Was the myanmar Earthquake?
The earthquake measured a magnitude of 7.7. This is the largest to strike Myanmar as 1912.
What Areas Were Affected by the Earthquake?
While the epicenter was in Myanmar, the earthquake’s effects were felt far and wide:
Myanmar: Extensive damage was reported, particularly in the Sagaing region.
Thailand: Neighboring Thailand also experienced the tremor, with reports of fatalities and building collapses in Bangkok.
China: The earthquake was also felt in parts of China.
Why Was the Earthquake So Destructive?
The shallow depth of the earthquake, less than 70 kilometers from the surface, amplified its destructive impact. As Roger Musson, a researcher at the British Geological Survey, explained, the shock waves didn’t dissipate as they moved from the epicenter to the surface, meaning buildings received the full force of the ground shaking.
What Type of Fault Caused the Earthquake?
The earthquake occurred along the Sagaing fault, a strike-slip fault. Strike-slip faults occur when tectonic plates slide horizontally past each other.
Is Myanmar Prone to Earthquakes?
Yes, Myanmar is situated on the border between two tectonic plates, making it one of the world’s most seismically active regions.
Joanna faure Walker,an earthquake expert at University College London,explained that this region is where the Indian and Eurasian plates meet. Thes plates move past one another horizontally.
How Does the Earthquake Compare to Previous Events?
The March 28, 2025 earthquake is considered the largest to hit Myanmar in the last 75 years. The last major earthquake in the Sagaing region was in 1956. Prior to this event,the largest event occurred in 1912.
What’s the Impact on infrastructure?
The infrequency of large seismic events in the Sagaing region suggests that infrastructure may not have been built to withstand strong shocks. This perhaps exacerbated the damage.
Key Facts and Figures in Summary:
| Feature | details |
| :————————- | :————————————————————————————————————– |
| Magnitude | 7.7 |
| Location | sagaing region, Myanmar |
| Fault Type | Strike-slip |
| Depth | Shallow (less than 70 km) |
| Deaths (as of March 29, 2025) | Over 1,000 |
| Impact in Thailand | Fatalities, building collapses |
| largest Earthquake | As 1912 |