| 1839 Ava earthquake | |
| Casualties: | 300–400 dead |
| Aftershocks: | Yes |
| Foreshocks: | Yes |
| Affected: | Konbaung dynasty (present–day Myanmar) |
| Fault: | Sagaing Fault |
| Magnitude: | 7.9–8.3 |
| Local-Time: | 04:00 |
| Local-Date: | 23 March 1839 |
| Timestamp: | 1839-03-23 24:30 |
| Location: | 21.9°N 96°W |
| Pre-1900: | yes |
The 1839 Ava earthquake, also known as the Amarapura earthquake or Inwa earthquake, was a disastrous seismic event that struck present-day central Myanmar on March 23.[1] This earthquake with an estimated moment magnitude as high as 8.3, was one of the largest in the country, since 1762. It was assigned a maximum of XI (Extreme) on the Modified Mercalli intensity scale, and was felt in Rangoon and Bhamo.[2] Damage was enormous in Ava, resulting in the death of hundreds.
Myanmar is wedged between four tectonic plates; the Indian, Eurasian, Sunda, and Burma plates, that interact due to active geological processes. Along the west coast of the Coco Islands, off the Rahkine coast, and into Bangladesh, is a highly oblique convergent boundary known as the Sunda megathrust. This large fault marks the boundary between the Indian and Burma plates. The megathrust emerges from the seafloor in Bangladesh, where it runs parallel and east of the Chin Hills. This boundary continues to north of Burma where it ends at the eastern Himalayas.[3]
The Sagaing Fault is a mostly continental transform fault that runs through Burma and connects the Andaman spreading center to the collision zone in the north. It accommodates motion between the Burma and Sunda Plates as they slide past each other at a rate of 18 to 49 mm/yr. The fault runs the entire length of the country for over 1,200 km and continues its trace into the Andaman Sea. The Sagaing Fault is Burma's largest and most active source of seismic threat, running through or close to major cities like Yangon, Nay Pyi Daw and Mandalay. Several large and damaging earthquakes have occurred on this fault in historical times. In 1946 the long Sagaing segment produced two major earthquakes but there are no records of its impact. Ten years later, in 1956, a magnitude 7.1 earthquake struck close to the city of Mandalay, re-rupturing the 1839 rupture zone for about .[4] Meanwhile, the long Meiktila segment has not experienced any major earthquake since 1839 and is considered a seismic gap.
The Meiktila and Sagaing segment of the fault ruptured during this earthquake for a length of, corresponding to a magnitude 8.1–8.3 earthquake, although little research has been conducted to provide further constrains.[5] On the basis for its overall lack of seismic activity, the Meiktila segment is believed to have ruptured during the earthquake. This segment runs from Nay Pyi Taw to Mandalay, a length of about .[6] [7] Remote sensing and field observation revealed a maximum displacement of along the trace of the 1839 rupture just outside Mandalay. This would place the magnitude at 7.4–8.0+ and generate a ~ rupture.[8] [9]
Researchers at National Taiwan University combined lidar and macroseismic data from historic accounts to estimate its magnitude at ~ 7.9 and rupture length to be . The 1839 earthquake ruptured two segments; the Meiktila segment in the south and Sagaing segment in the north. They estimated of displacement on the Sagaing segment while slip on the Meiktila segment was around . The felt area based on the Modified Mercalli intensity was larger than the 1912 Maymyo earthquake (7.7) and similar in area to the 2002 Denali earthquake (7.9). The maximum assigned Modified Mercalli intensity was XI (Extreme).[10]
The mainshock was preceded by a large foreshock in 1838, which also damaged the capital.[11] Great damage was reported in Inwa, so severe that the formal capital was moved to nearby Amarapura. In Mingun, a stupa sustained serious damage as a result of shaking. British officials in Myanmar recorded catastrophic damage and liquefaction in Mandalay and the surrounding area.[12] [13] Many pagodas collapsed during the event. Chasms and fissures more than wide were seen in Amarapura and nearly every brick building was reduced to rubble. Some villages were swallowed up as a result of liquefaction. By a contemporary British estimate, about 300–400 people died.[1] The shock also reversed the flow of the Irrawaddy River, where the currents became violent and overflowed its banks. It was felt for thousands of miles away from the epicenter, as far as Dhaka, Kolkata, and Bangkok.