Significant earthquakes of 2013

July 2, 2013 Earthquake: Banda Aceh, Indonesia

July 2, 2013 · M6.1 · 48 deaths · $113 million · 20,401 houses destroyed

A magnitude 6.1 earthquake struck Banda Aceh, Indonesia on July 2, 2013 at 07:37:02 UTC, 13 km below the surface. It killed 48 people.

Map

Where it struck, with the other significant earthquakes within 200 km. Circles are sized and colored by magnitude; select one for its page.

The earthquake

Date
July 2, 2013
Time
07:37:02 UTC
Place
Banda Aceh, Indonesia
Magnitude
6.1 (Mw)
Focal depth
13 km (8 mi)
Tsunami
None recorded
Epicenter
4.645° N, 96.665° E
Country
Indonesia

The toll

Deaths
48
Injuries
2,532
Damage
$113 million
Houses destroyed
20,401

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

Felt Reports

At least 42 people killed, 2,500 injured, 6 missing and 53,339 displaced and 20,401 buildings destroyed or damaged in the Bener Meriah-Central Aceh area. One person killed by a landslide in Bener Meriah. Several landslides damaged roads, cutting off access to 9 villages. Felt (IV) at Banda Aceh, Lhokseumawe and Takengon and (III) at Medan. Felt (III) at Georgetown and Gelugor, Malaysia. Also felt at Ayer Itam, Balakong, Butterworth, Petaling Jaya, Sungai Ara and Tanjong Bunga. Felt at Phuket, Thailand.

Tectonic SummaryThe M 6.1 July 2, 2013 earthquake south of Bireun, Indonesia occurred as a result of strike slip faulting within the crust of the Sunda plate. The earthquake struck several hundred kilometers to the east of the Sunda-Java Trench, which is the seafloor expression of the plate boundary between Sunda and the Indo-Australia tectonic plates. The location and faulting mechanism of this earthquake are consistent with upper plate accommodation of the right-lateral component of oblique convergence between the two plates, which is most clearly expressed along the Sumatran Fault, a major transform structure that bisects the island of Sumatra and whose main strand lies further to the west of the July 2 earthquake. At the latitude of this event, the Indo-Australia plate moves towards the northeast with respect to Sunda at a rate of approximately 60 mm/yr.

While earthquake activity in the region is more frequently associated with thrust faulting along the subduction zone to the west of the July 2 earthquake, upper plate events in Sumatra have not been uncommon; half a dozen M6+ earthquakes have occurred within 250 km of the July 2 event over the past 40 years. Such earthquakes can be very hazardous if close to population centers - as the July 2 event was - because of their shallow depths. A M 6.7 earthquake in November 1990, 120 km to the southeast, resulted in approximately 7 fatalities.

(above from reference #1053)

Jakarta (ANTARA News) - The National Disaster Mitigation Agency (BNPB) on Sunday reported that the death toll of the earthquake in Aceh had increased to 40 from 30 as previously reported on Thursday. Spokesperson of BNPB Sutopo Purwo Nugroho on an official statement on the agency website said that as many as 2,362 people were injured, 63 were heavily injured while the other 22,125 were displaced due to the earthquake. The magnitude 6.2 earthquake cast damage to over 15,919 residential houses and 623 public buildings. Central Aceh District becomes the most affected by the earthquake with 31 dead casualties, four residents missing, and the other 19,879 were displaced and taking refuge to 70 camps spread across the district. As many as 232 out of 352 villages in the district suffered the most damage by the earthquake. The earthquake damaged 13,862 resident houses; 5,516 with heavy damage, 2,750 suffered medium damage, and 5,596 with minor damage, and also 547 public buildings such as health center buildings, schools, and administration buildings. Meanwhile in Bener Meriah District, there are only eight of 233 villages directly affected by the earthquake. The Agency reported nine resident were dead, 23 injured and 2,265 displaced due to the earthquake. There refugees needed more supply of tents and blanket as they were evacuated to makeshift camps in mountainous area in which the temperature hit 14 degree Celsius at night, Nugroho said. The earthquake cast damage to 2,057 resident houses; 662 were heavily damaged, 311 with medium damage and 1,184 with minor damage, and 76 public facilities. (reference #10658)

42 dead, 6 missing, 558 injured, 113m USD total damages (reference #13045)

48 deaths, 2532 injured, 130m USD total damages (reference #1250)

Other significant earthquakes nearby

Within 200 km, the deadliest first.

More

Significant earthquakes of 2013The 2000sEvery quake the USGS located in 2013Recent earthquakes near hereThis day in weather history

Sources

Significant earthquakes from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI earthquake 10005.