On March 28, 2025, a powerful magnitude 7.7 earthquake struck near Mandalay, Myanmar, sending tremors across much of Southeast Asia and causing widespread destruction in Myanmar while shaking buildings as far away as Bangkok. The quake occurred at a shallow depth of about 10 kilometers, a factor that amplified the intensity of shaking at the surface and contributed to the extensive damage.
The epicenter was close to Mandalay, Myanmar’s second-largest city, in a region dominated by active fault systems, particularly the Sagaing Fault, where strike-slip motion can trigger major earthquakes. When a quake of this size happens at such a shallow depth, ground movements are sharp, rapid, and especially destructive to structures not designed for strong lateral shaking.
Residents in Mandalay and nearby towns described being jolted awake by rolling waves of ground movement. In seconds, glass shattered, walls cracked, and heavy objects toppled. People ran into the streets in whatever they were wearing—some barefoot, some holding children, others wrapped in blankets—seeking open space away from buildings that had suddenly become dangerous. Amid the dark and dust, alarms, car horns, and shouting mingled with aftershocks that continued to rattle nerves and weaken already damaged structures.
The quake’s effects extended beyond Myanmar’s borders. Tremors were felt in Thailand, including in Bangkok, where skyscrapers swayed noticeably. Long-period ground motion caused taller buildings to move more than expected, even at a considerable distance from the epicenter. In southwestern China’s Yunnan province, near the Myanmar border, authorities reported damage and injuries in towns such as Ruili. The incident highlighted that earthquakes ignore political boundaries—communities far from the epicenter can still face serious consequences.
Emergency response became an urgent race against time. Communications were disrupted, roads damaged, and access to rural areas hampered by landslides and debris, slowing rescue operations. Hospitals and clinics faced surges of injured patients, dealing with fractures, head trauma, and crush injuries while also coping with power outages and staff worries about their families. Most injuries after earthquakes come from falling debris or accidents while fleeing unsafe buildings, and older or poorly reinforced structures are especially vulnerable.
Aftershocks added another layer of danger. Even weeks or months after the main quake, strong jolts could topple weakened buildings, keeping residents on edge and disrupting sleep. Hundreds of aftershocks were reported in the weeks following the event.
Initial casualty figures were uncertain but rose as rescue teams reached more remote locations. Search-and-rescue teams worked under physically demanding and emotionally taxing conditions, using sniffer dogs, drones, and heavy equipment where possible. Small rescues became powerful symbols of hope, demonstrating survival was still possible despite extensive destruction. Authorities urged people to avoid damaged structures and remain vigilant for secondary hazards such as gas leaks, fires, unstable walls, and landslides.
Beyond the immediate aftermath, the earthquake exposed long-term challenges: providing shelter for displaced families, restoring water and electricity, and rebuilding safely. Reconstruction requires balancing speed, cost, and stricter safety standards, a difficult task in regions where governance and resources are limited.
The March 28, 2025 earthquake was among the strongest Myanmar has experienced in over a century. Its combination of magnitude, shallow depth, and proximity to population centers produced intense shaking and widespread impact, with recovery expected to take years rather than weeks.