2005 Kashmir earthquake: October 8 2006 6.4 Indonesia, Yogyakarta: 10.0 IX: At least 28,903 people were killed, 137,883 were injured and as many as 779,287 people were displaced in the Bantul-Yogyakarta area. Merapi activities was increasing. May 27, 2006 YOGYAKARTA, Indonesia, Saturday, May 27 (AP) — A powerful earthquake rocked Indonesia's Central Java province early Saturday, killing at least 291 people and injuring scores . and aftershock data of the 2006 M6.3 Yogyakarta earthquake Hijrah Saputra1, Wahyudi Wahyudi 1, Iman Suardi2, Ade Anggraini1 and Wiwit Suryanto1* Abstract This study comprehensively investigates the source mechanisms associated with the mainshock and aftershocks of the Mw = 6.3 Yogyakarta earthquake which occurred on May 27, 2006. Indonesia: Earthquake, Yogyakarta and Central Java - Emergency Situation Report Number 9 was issued by the World Health Organization through Relief Web on June 6, 2006. Many stones were dislodged and some parts broke off during the earthquake, and civil engineers were brought in to investigate the characteristics of the soil under the temple using ground penetrating radar, bore samples, and standard penetration tests. No surface breaks were documented, but the location of the greatest damage that was caused does align with the Opak Fault as a possible source. With 66,000 homes destroyed, the Klaten District saw the heaviest damage, followed by Bantul, with 47,000 destroyed. Share. The 2006 Yogyakarta earthquake (also known as the Bantul earthquake) occurred at 05:54 local time on 27 May with a moment magnitude of 6.4 and a maximum MSK intensity of VIII (Damaging). GLIDE No. The type and properties of sediment control the occurrence and distribution of liquefaction, and other environmental conditions (like the water table) also play a part, as well as the peak ground acceleration of the earthquake. In 2006, a large earthquake shocked the denselypopulated Yogyakarta Province and its surrounding areas. Found insideThese events have created new and detailed casualty data, which has not until now been properly assembled and evaluated. This book draws the new evidence from recent events together with existing knowledge. Borehole and magnetic data surveys show that the alluvium and lahar deposits at the Bantul graben are 20–200 meters (66–656 ft) thick and at places over 200 meters, and the water table is .6–5 meters (2 ft 0 in–16 ft 5 in) below ground level. Sedimentation is closely related to tectonics, and while the volume of offshore sediment at the trench decreases with distance from the Ganges-Brahmaputra Delta at the Bay of Bengal, the onshore accrual of sediments near the Special Region of Yogyakarta has been shaped by tectonic events. (a) Location map. [23] stated that there are several versions of the location of the epicenter. This study may be the first application of InSAR to seismogenic fault identification of the 2006 Yogyakarta earthquake, although Matsuoka and Yamazaki (2006) applied a damage detection This earthquakecaused huge fatalities and damaged thousands of buildings andinfrastructures. The earthquake of moment magnitude, Mw 6.3 in Yogyakarta and Central Java on May 27, 2006 caused widespread death and destruction to the heavily populated and relatively prosperous region. The epicentre was located approximately 37 km south of the city of Yogyakarta. A powerful earthquake rattled Yogyakarta, Java, Indonesia, in the early morning hours of May 27, 2006. [14], The Prambanan Temple Compounds (also known as the Roro Jonggrang Temple) was constructed near the border of Yogyakarta and Central Java in 856, and was abandoned shortly thereafter. This was the fifth major disaster caused by earth movement in recent years starting with the Tsunami in 2004, Yogyakarta in 2006, Padang in 2009, Palu in 2018 and Lombok in 2019. The Opak fault, a fault mapped by geologists was thought to be the source of this earthquake disaster. Most liquefaction events took place near the 2.5 km (1.6 mi) wide Opak Fault zone. Merapi volcanic: did lahar deposits amplify ground shaking and thus lead to the disaster?," An Electronic Journal of the Earth Sciences, 9, 5 (2008). Map of groundwater level and location of site investigation Figure 5. Flight Center. Equal to the maximum ground acceleration that occurred during earthquake shaking at a location. This paper focuses on the local economic growth impacts of a specific natural disaster, viz. The ASTER sensor on NASA’s Terra satellite captured an image of the volcano in action on June 6. More than 2,000 residents of Bantul were killed, thousands of its residents injured, and 80% of its homes damaged or destroyed. Of the three home construction styles used in the area, the most common type fared badly. Ref: OCHA/GVA - 2006/0151 OCHA Situation Report No. The earthquake occurred along a fault east of the mountains that frame Yogyakarta to the east. The earthquake is not the only geologic activity to threaten the region: the Merapi volcano was also rumbling at the end of May. With limited effects to public infrastructure and lifelines, housing and private businesses bore the majority of damage (the 9th-century Prambanan Hindu temple compound was also affected), and the United States' National Geophysical Data Center classified the total damage from the event as extreme. Land. The subduction zone offshore Java is characterized by a northward dipping Benioff zone, frequent earthquakes and volcanic activity that influence the regional geography, and direct or indirect stress transfer that has affected the various onshore faults. The earthquake impacted five districts within Daerah Istimewa Yogyakarta (DIY), the Special Region of Yogyakarta and six districts within the neighbouring province of Central Java. The shock had a moment magnitude of 7.7 and a maximum perceived intensity of IV (Light) in Jakarta, the capital and largest city of Indonesia. On May 27, 2006, a magnitude 6.3 earthquake on the moment magnitude scale and lasted for 52 seconds struck Central Java and Yogyakarta, center for Javanese traditional arts and culture as well as a center of Indonesian higher education. Left: events before May 2006 since 1971. 2 on the Richter scale (2) devastated the provinces of Yogyakarta and Central Java, killing about 6000 people, injuring another 40 000-60 000 and robbing hundreds of thousands of their homes and livelihood (3). 2).According to the Bappenas report, this earthquake, which had a strength of 5.9 on the Richter scale (or 6.3 according to the USGS), was one of the most . The Pacitan region is geographically close to Yogyakarta, and is located only 120 km from the epicenter of the quake. The south central portion of the island of Java (one of the five largest in the Indonesian archipelago) had been affected by an eruption of Mount Merapi that began prior to the May 27 earthquake, but the Special Region of Yogyakarta has experienced numerous other . Found insideThis volume attempts to answer such fundamental concerns as why some interplate subduction earthquakes are relatively modest in rupture length (greater than 100 km) while others, such as the great (M greater than 9) 1960 Chile, 1964 Alaska, ... Google Scholar; 13. Yogyakarta 2006 earthquake point (Source: Commons Wikimedia) Quoting the Kompas report, there were 3,098 victims who were killed and 2,971 of them came from Bantul Regency on Saturday 27 May 2006 until 00.15 WIB. The Mw6.4 May 26, 2006 Yogyakarta Earthquake caused severe damage and claimed more than 5,000 lives in Bantul district of the Yogyakarta Special Province and Klaten District of Central Java Province. Damage in central Java was more pronounced because of the substandard construction practices and the high population density, but on the other end of the scale, damage to infrastructure was very limited. Found inside – Page 127... OF BANTUL FROM THE 2006 YOGYAKARTA EARTHQUAKE1 TADJUDDIN NUR EFFENDI, ... examines the impact of the 2006 Central Java and Yogyakarta earthquake, ... 1. Earthquake mitigation plan in the area has been carried out by understands the location of the fault. The Yogyakarta earthquake: testing the IFRC'S decentralized supply chain3.1. Yogyakarta sits in a broad valley between two groups of roughly north-running mountains. 100% (1/1) Merapi Gunung Merapi massive eruption of Mount Merapi. Missing Not specified This unconsolidated material from the stratovolcano amplified the intensity of the shaking and created the conditions for soil liquefaction to occur. Researchers stated that the Yogyakarta region is seismically active, with four known events in the 19th century and three in the 20th century, with peak ground acceleration values of 0.038–0.531g. This image shows bathymetry in shades of blue and topography in shades of brown in the area where an earthquake struck off the shore of western Java on September 2, 2009. Hundreds of thousands of people were left homeless. Image of the Day Found inside – Page 56Measured at 6.4 on the Richter scale, the 2006 Yogyakarta earthquake sent shudders ... 60 Over the next few weeks, archaeologists sifted through the damage; ... YOGYAKARTA, Indonesia, May 28 — The death toll rose today from the powerful earthquake that struck early Saturday, and aid agencies poured into devastated areas as rescue workers . Over 5,500 people were killed in the immediate aftermath . A unique interdisciplinary approach to disaster risk research, including global hazards and case-studies, for researchers, graduate students and professionals. The images are thumbnails, click for full view. The volcano sent clouds of hot gas and lava down its slopes on June 6, prompting the evacuation of 11,000 people, said news reports. Found inside – Page 277Deadliest natural disasters (2000-2019) Year Death toll Event Location 2000 800 ... 2005 Kashmir earthquake Pakistan 2006 5,782 2006 Yogyakarta earthquake ... Of nine events that were analyzed, it was found that the station at Imogiri (a heavily affected village that was built on 150–200 meters (490–660 ft) of sediment) showed signs of local amplification when compared to a location that was built on bedrock, and that the deposits amplified the impact of the shallow crustal rupture. George Ho 03:33, 16 May 2015 (UTC) Dawnseeker2000 02:46, 7 May 2015 (UTC) Main Source http://www.who.or.id/eng/php/content/jogja-centraljava/Sitrep%20Indonesia%20Jogja-Central%20Java%2004-06-06%20(7).pdf The 26 May 2006 teleseismic locations and focal mechanisms are provided by Bantul Regency was the region most affected by the disaster. Found inside – Page 40Harris and Ripepe (2007) report changes in eruption rate at Semaru volcano, Indonesia in response to the 2006 M6.3 Yogyakarta earthquake based on satellite ... The strongest foreshocks (M5.5-5.6) occurred on July 1st at 11:34 am ADT, and on July 2nd at 8:57 am and 9:20 am ADT. The epicentre was located approximately 37 km south of the city of Yogyakarta. Brief Overview of the Disaster  [13], With 154,000 houses destroyed and 260,000 units experiencing damage, the event was one of the most costly natural disasters in the previous ten years. Source Model of the 2007 Mw 8.0 Pisco, Peru earthquake — implications for seismogenic behavior of subduction megathrusts. Microtremor survey was conducted together with boring survey for the determination of site amplification and strong ground motion characteristics in southern Yogyakarta Depression, Indonesia. 1-D dynamic response analysis by equivalent ... 2006 Yogyakarta earthquake. 2006 Yogyakarta earthquake. 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