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| UTC time | 2000-06-04 16:28:26 |
|---|---|
| ISC event | 1736014 |
| USGS-ANSS | ComCat |
| Local date | June 4, 2000 |
| Local time | 23:28 |
| Magnitude | 7.9 Mw [1] |
| Depth | 35 km (22 mi) [1] |
| Epicenter | 4°37′S 102°04′E / 4.61°S 102.06°E [1] |
| Type | First subevent strike-slip Second subevent megathrust[2] |
| Areas affected | Indonesia |
| Max. intensity | VI (Strong) [3] |
| Aftershocks | 6.7 Mw June 4 at 16:39 [4] |
| Casualties | 103 dead [5] 2,174–2,585 injured [5] |
At 23:28 local time on June 4, 2000 southern Sumatra, Indonesia was struck by an earthquake of moment magnitude 7.9 with a maximum Mercalli intensity of VI (Strong). The event occurred off the coast near Enggano Island. There were more than 100 fatalities and up to 2,585 injuries. Over 730 aftershocks shook the area afterwards, one just eleven minutes after the mainshock.
This was the first and southernmost in a series of very large to great Sumatran earthquakes in the 2000s to rupture almost the entire western part of the Sunda megathrust, most notably including the 9.1–9.3 2004 Indian Ocean earthquake, but also the 8.7 2005 Nias–Simeulue earthquake, and the 7.9–8.4 September 2007 Sumatra earthquakes.
Indonesia is well known for strong earthquakes: the 2000 Enggano event marked the beginning of an ongoing period of seismic activity in the area, highlighted by the 2004 Indian Ocean earthquake. The 2000 Enggano earthquake took place at the southeastern end of the fault segment that ruptured during the 1833 Sumatra earthquake. This group of earthquakes, in addition to the 2005 Nias–Simeulue earthquake, all ruptured along the megathrust that forms the interface between the Australian and Sunda Plates.[6] This event was the only one not to cause a tsunami.
The earthquake involved the rupture of two different faults with different mechanisms. The first subevent ruptured a north–south striking fault within the Australian Plate with a left lateral strike-slip mechanism. The earthquake rupture propagated northwards until it reached the megathrust, triggering the second subevent along the Sunda megathrust itself. The strike-slip rupture probably represents slip on a pre-existing fracture zone, similar to the likely cause of the M 7.9 earthquake that struck about 1,000 km to the south on 18 June 2000 with a similar mechanism.[2]
At least 46 people were killed, 940 were injured and 1,008 affected houses were reported in the Bengkulu area. Thirty-nine deaths, 1,245 injuries and 90 percent of houses were destroyed on Enggano Island.[7] In the village worst struck, several hundred structures were reported in ruins.[8][9] An aftershock measuring 6.2 struck on June 7.[10]
International relief teams arrived in the region within several days.[11] Relief efforts were impeded by fallen telephone poles, which blocked the supplies.[8] The main problem found in the affected areas was a lack of water supply and electricity, these facilities having been cut off by oscillation.[8] Pope John Paul II expressed his "sincere sympathy" for those families stricken by the earthquake.[12] He called for a rapid international response to the quake, and said he would keep its victims in his prayers.[12] A Taiwanese rescue team was sent to help victims of the tremor, the first country to take part in rescue efforts from Asia. The United States donated US$ 25,000 instantly to relief organizations, Japan offering a grant of US$140,000 and Australia US$143,000 in addition to a two-person team of emergency relief examiners.[13]
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| UTC time | 2000-06-18 14:44:13 |
|---|---|
| ISC event | 1736624 |
| USGS-ANSS | ComCat |
| Local date | June 18, 2000 |
| Local time | 22:44 |
| Magnitude | 7.9 Mw |
| Depth | 10 km (6.2 mi) |
| Epicenter | 13°48′07″S 97°27′11″E / 13.802°S 97.453°E |
| Type | Intraplate |
| Areas affected | Indonesia |
| Max. intensity | II (Weak)[14] |
| Tsunami | 0.3 m (0.98 ft)[14] |
| Aftershocks | 17 (As of June 27 2000)[15] |
| Casualties | None |
Two weeks later on June 18, another magnitude 7.9 event occurred about 1,000 kilometers (620 mi) to the southwest in the Wharton Basin. At the time, it was the largest intraplate earthquake in the Indian Ocean until the 2012 Indian Ocean earthquakes.[2]