2021 Bali earthquake

Last updated

2021 Bali earthquake
Indonesia Bali location map.svg
Bullseye1.png
Indonesia relief location map.jpg
Bullseye1.png
UTC  time2021-10-15 20:18:20
ISC  event 621204453
USGS-ANSS ComCat
Local date16 October 2021 (2021-10-16)
Local time04:18 WITA
Magnitude4.7 Mw
Depth10.0 km (6.2 mi)
Epicentre 8°20′53″S115°27′40″E / 8.348°S 115.461°E / -8.348; 115.461 Coordinates: 8°20′53″S115°27′40″E / 8.348°S 115.461°E / -8.348; 115.461
Type Strike-slip
Areas affected Indonesia
Max. intensity IV (Light) (BMKG) [1]
LandslidesYes
Casualties4 dead, 73 injured [2]

The 2021 Bali earthquake struck at 04:18 local time (UTC+08:00) when people were still sleeping on 15 October 2021. It resulted in 4 deaths and 73 more injured, despite having a moment magnitude of 4.7. [3]

Contents

Tectonic setting

The island of Bali forms part of the Sunda Arc, which formed above the convergent boundary where the Australian Plate is subducting beneath the Sunda Plate. The rate of convergence across the line of the SundaJava Trench is 7.5 cm per year. Eastwards from Bali, the Sunda Arc is also being thrust over the Bali and Flores back-arc basins on a series of south-dipping thrusts. Focal mechanisms of earthquakes near Bali are dominantly thrust sense on both the subduction interface and the system of thrust faults to the north. [4] In July and August 2018, a series of earthquakes, the strongest reaching 6.9 on the moment magnitude scale, killed nearly 600 people in the neighbouring island of Lombok. [5] [6] [7] [8] [9] In January 1917, an earthquake measuring 6.6 killed more than 1,500 people, 80% of which from landslides.

Earthquake

According to officials at the Meteorology, Climatology, and Geophysical Agency (BMKG), the earthquake, which was centred at the sloped of the volcanoes Mount Agung and Mount Batur, occurred on a shallow local fault. Rupture along the fault was caused by the migration of magma in the crust, triggering fault activity. The BMKG has ruled out the Flores Back Arc Thrust Fault as the source of the quake due to the strike-slip focal mechanism indicated by the seismological data. [10] [11]

Instrumental seismic intensities measured by the BMKG suggest the quake only caused light shaking in Bali, but was felt as far as Lombok. [12] At Denpasar, Karangasem, and northern Lombok the earthquake was felt lightly by residents at IV on the Mercalli intensity scale. [1]

Impact

Most of the damage was observed in the Ban Village, Kubu District, Ppatan Village, Rendang District and Karangasem Regency. Many religious and historical structures were mildly to severely damaged. Four people were confirmed dead, one of them being a three-year-old girl who was hit by falling debris. The other three deaths were from a landslide. [2] [13] Seventy-three people were injured, suffering head injuries or broken bones. Most of the injured were treated at the Kubu Pratama and Karangasem hospitals where they were discharged. Three remained hospitalized for their serious injuries. At least 762 buildings were damaged, 101 of which were religious. [14]

See also

Related Research Articles

<span class="mw-page-title-main">Great Sumatran fault</span> Geological feature

The Indonesian island of Sumatra is located in a highly seismic area of the world. In addition to the subduction zone off the west coast of the island, Sumatra also has a large strike-slip fault, the Great Sumatran Fault also known as Semangko Fault, running the entire length of the island. This fault zone accommodates most of the strike-slip motion associated with the oblique convergence between the Indo-Australian and Eurasian plates. The fault ends in the north just below the city of Banda Aceh, which was devastated in the 2004 Indian Ocean earthquake. After the December 2004 earthquake, pressure on the Great Sumatran Fault has increased tremendously, especially in the north.

The 1979 Bali earthquake occurred at 03:58 local time on 18 December with a surface wave magnitude of 6.3. The shock occurred southeast of the coast of Karangasem Regency in the Lombok Strait, and about 60 kilometres (37 mi) east-northeast of Denpasar. Up to 80 percent of the buildings in Karangasem Regency were damaged, between 15,000 and 500,000 people were displaced, and road links to the provincial capital of Denpasar were briefly severed.

The 1976 Bali earthquake occurred at 15:13 local time on 14 July with a surface wave magnitude of 6.5. The shock occurred 5 kilometres (3.1 mi) south of the Bali Sea coast of the Buleleng Regency, and about 65 kilometres (40 mi) northwest of Denpasar. Up to ninety percent of houses in Buleleng Regency were seriously damaged or destroyed and the Seririt sub-district was almost completely destroyed, where a school building collapsed and trapped at least 200 students. 573 people are believed to have died; at least 544 in Buleleng Regency, 24 in Jembrana and 5 in Tabanan. Four thousand more suffered injuries and an estimated 450,000 were left temporarily homeless.

<span class="mw-page-title-main">July 2018 Lombok earthquake</span> Earthquake that occurred in July 2018 in Indonesia

A Mw 6.4 earthquake struck the island of Lombok on the morning of 29 July 2018 at a shallow depth of 14 km (8.7 mi). Widespread damage was reported in the area, and authorities confirmed that 20 people were killed in the earthquake while hundreds were injured.

<span class="mw-page-title-main">5 August 2018 Lombok earthquake</span> Earthquake that occurred on August 5, 2018 in Indonesia

On 5 August 2018, a destructive and shallow earthquake measuring Mw 6.9 struck the island of Lombok, Indonesia. It was the main shock following its foreshock, a nearby Mw  6.4 earthquake on 29 July. It was followed by a nearby 6.9 earthquake on 19 August 2018.

<span class="mw-page-title-main">19 August 2018 Lombok earthquake</span> Earthquake in Indonesia

On 19 August 2018 a major earthquake struck with high intensity on the northeast corner of Lombok and northwest Sumbawa at 22:56 local time, a few km to the east of the series of quakes that had been rocking the area for the past 3 weeks. It was measured at Mw  6.9 (USGS), at a depth of 25.6 km. The Indonesian BMKG announced that it was a new major earthquake and it was not an aftershock. The earthquake occurred on the same overall structure, the Flores Back Arc Thrust Fault, however according to scientists it happened on a different thrust fault as there are many individual structures within the belt. There were 14 deaths and 1800 homes have been damaged, half severely, due to this event, including deaths on Sumbawa, following 2 deaths from the previous Lombok quake roughly 24 hours earlier. Heavy tiles fell from the local mosque, and 143 patients were being treated outdoors in makeshift tents for injuries on Sumbawa.

Flores Back Arc Thrust Fault is a major system of west-east trending thrust faults that extend eastwards from west of Lombok towards the islands of Sumbawa, Flores, and Alor, with a total length of at least 800 km. The thrust faults are south-dipping and lie within the back arc region of the Sunda-Banda Arc, which is related to the ongoing subduction of the Australian Plate beneath the Sunda and Banda Sea Plates. The thrust fault system developed as a result of the onset of continental collision as continental crust of the Australian Plate reached the Sunda Trench. The eastern part of the fault system is also known as the Wetar thrust. Above the main thrust fault are a series of imbricate (overlapping) thrust faults. These imbricate thrust faults are shallower in depth than the main Flores thrust. Although the exact thrust faults have not been established, these faults were thought to be responsible for the 2018 Lombok earthquakes.

<span class="mw-page-title-main">2018 East Java earthquake</span> Earthquake affecting Indonesia

On 11 October 2018, an earthquake struck off the coast of East Java, Indonesia, with the epicentre located off the coast of Situbondo Regency. The earthquake, which struck at dawn, killing four people in addition to destroying or damaging hundreds of houses, mostly on the small island of Sapudi.

On 17 March 2019, an earthquake measuring Mw  5.6 struck the island of Lombok in West Nusa Tenggara, Indonesia. The earthquake triggered a landslide, killing six and injuring nearly 200 others.

<span class="mw-page-title-main">2019 Sunda Strait earthquake</span> 7 July 2019, earthquakes in Indonesia

The 2019 Sunda Strait earthquake occurred on the night of 2 August 2019, when a magnitude 6.9 earthquake rattled Sunda Strait at a moderate depth of 52.8 kilometres. The epicentre was located 214 km from Bandar Lampung, the capital of Lampung and 147 km west of Sumur, Pandeglang Regency. The earthquake struck with a maximum intensity of VI (Strong). The earthquake prompted a tsunami warning in the area, with authorities urging coastal residents to immediately evacuate to higher grounds.

An earthquake struck Majene Regency in the province of West Sulawesi, on the Indonesian island of Sulawesi on 15 January 2021, at 02:28 WITA, with a moment magnitude of 6.2. This earthquake was felt as far away as Makassar, the capital of South Sulawesi, and Palu in Central Sulawesi. Strong shaking was reported in Majene and the provincial capital Mamuju for at least 5–7 seconds. It was preceded by a foreshock measuring 5.7 magnitude a few hours earlier.

The 1674 Ambon earthquake occurred on February 17 between 19:30 and 20:00 local time in the Maluku Islands. The resulting tsunami reached heights of up to 100 metres (330 ft) on Ambon Island killing over 2,000 individuals. It was the first detailed documentation of a tsunami in Indonesia and the largest ever recorded in the country. The exact fault which produced the earthquake has never been determined, but geologists postulate either a local fault, or a larger thrust fault offshore. The extreme tsunami was likely the result of a submarine landslide.

<span class="mw-page-title-main">2021 East Java earthquake</span> Earthquake in Indonesia

An earthquake occurred on 10 April 2021 at 14:00 local time (UTC+07:00) off the south coast of eastern Java. The epicenter of the earthquake is located 44 km south southwest of Gondanglegi Kulon in East Java province. Measuring 6.0 or 6.1 on the moment magnitude scale (Mw ) and having a depth of 82.3 km, the earthquake caused moderate shaking measuring V on the Mercalli intensity scale. At least 10 individuals are known to have died from the earthquake and another 104 were seriously injured.

<span class="mw-page-title-main">Lembang Fault</span> Fault in Indonesia

The Lembang Fault is an active fault located 10 km north of the city of Bandung on the Indonesian island of Java. This sinstral slip fault is estimated to measure 29 km in length. While no historical earthquakes have occurred, the fault is thought to be possible of generating a magnitude 6.5 to 7.0 earthquake in the future. Because of the potential for large and damaging earthquakes on the fault, the Meteorology, Climatology and Geophysics Agency (BMKG) has been monitoring activity on the fault.

<span class="mw-page-title-main">1995 Kerinci earthquake</span> Earthquake in Indonesia

The 1995 Kerinci earthquake struck near Sungai Penuh in Jambi Province on the island of Sumatra, Indonesia. It earthquake occurred at 01:18 WIB local time on October 7. The earthquake measured 6.7 Mw on the moment magnitude scale, and 6.9–7.0 Ms on the surface wave magnitude scale. Between 84 and possibly even 100 people were killed in the earthquake. An extimated 4,000 buildings collapsed or were seriously damaged while a further 5,000 suffered some damage.

The 1815 Bali earthquake occurred on November 22 between 22:00 and 23:00 local time (WITA), affecting the Bali Kingdom. The estimated moment magnitude 7.0 earthquake struck off the north coast of Bali at a shallow depth. It was assigned a maximum intensity of IX (Violent) on the Mercalli intensity scale, causing severe damage in Buleleng and Tabanan. The earthquake caused a landslide and tsunami that killed 11,453 people.

<span class="mw-page-title-main">2021 Flores earthquake</span> Earthquake in Indonesia

An earthquake occurred 112 km, offshore, north of Maumere in the Flores Sea on December 14. The quake had a moment magnitude of 7.3 according to the United States Geological Survey (USGS). One person was killed and 97 others suffered injuries.

<span class="mw-page-title-main">2022 Sumatra earthquake</span> Earthquake in Indonesia

On 25 February 2022, a magnitude 6.1 earthquake struck West Sumatra, Indonesia. According to the U.S. Geological Survey, the earthquake struck at a depth of 4.9 kilometres (3.0 mi) and had an epicenter in Pasaman. At least 19 people died, 425 were injured, and four others were missing. Severe damage occurred in Tigo Nagari District, Pasaman.

References

  1. 1 2 "Pusat gempa berada di darat 8 km barat laut Karangasem". bmkg.go.id. Meteorology, Climatology, and Geophysical Agency. 16 October 2021. Retrieved 16 October 2021.
  2. 1 2 "Risklayer Explorer". risklayer.com.
  3. "M 4.7 - Bali region, Indonesia". earthquake.usgs.gov. U.S. Geological Survey. 16 October 2021. Retrieved 16 October 2021.
  4. McCaffrey, R.; Nabelek J. (1987). "Earthquakes, gravity, and the origin of the Bali Basin: an example of a nascent continental fold-and-thrust belt" (PDF). Journal of Geophysical Research. 92 (B1): 441–460. Bibcode:1987JGR....92..441M. doi:10.1029/jb092ib01p00441. Archived from the original (PDF) on 11 December 2013. Retrieved 10 November 2012.
  5. "M 6.4 - 5km WNW of Obelobel, Indonesia". earthquake.usgs.gov. Retrieved 15 October 2021.
  6. "M 6.9 - 0km SW of Loloan, Indonesia". earthquake.usgs.gov. Retrieved 15 October 2021.
  7. "M 5.9 - 3km SE of Todo, Indonesia". earthquake.usgs.gov. Retrieved 15 October 2021.
  8. "M 6.3 - 6km NE of Sembalunlawang, Indonesia". earthquake.usgs.gov. Retrieved 15 October 2021.
  9. "M 6.9 - 2km S of Belanting, Indonesia". earthquake.usgs.gov. Retrieved 15 October 2021.
  10. Reza Yunanto (16 October 2021). "Analisis Penyebab Gempa Bali Hari Ini, Dipicu Aktivitas Sesar Patahan Lokal" [Analysis of the Causes of the Bali Earthquake Today, Triggered by Local Fault Activity]. iNewsBali.id. Retrieved 16 October 2021.
  11. "Memperhatikan mekanisme sumber Gempa Bali M4,8 yang merusak pagi ini, tampak bahwa gempa yang terjadi diakibatkan oleh aktivitas sesar/patahan aktif lokal, bukan akibat aktivitas Sesar Naik Flores (Flores Back Aec Thrusting)". twitter.com. @DaryonoBMKG. Retrieved 16 October 2021.
  12. Rizal Setyo Nugroho, ed. (16 October 2021). "Gempa Bali M 4,8 Dirasakan hingga Lombok" [Bali Earthquake M 4.8 Felt to Lombok]. Kompas. Retrieved 16 October 2021.
  13. "Earthquake of magnitude 4.8 strikes Bali, kills three". Reuters. Retrieved 15 October 2021.
  14. "Gempa Karangasem, 1 Meninggal Dunia, 71 Korban Luka, Ratusan Rumah di Desa Ban Rusak Berat" (in Indonesian). Bali Factual News. 16 October 2021. Retrieved 16 October 2021.