2006 yogyakarta earthquake location

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. Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3.1 billion). On 2006 May 26 at 23:54 UTC, a moderate shallow crustal earthquake with a moment magnitude of 6.3 occurred in the southern part of Yogyakarta in Java, Indonesia. [8], A group of Japanese and Indonesian scientists visited the area in March 2007 and confirmed the lack of surface ruptures, and pointed out that any visible expression of the fault would likely have been rapidly destroyed due to the tropical climate, and have acknowledged the widely varying locations (and the preference for the Opak Fault) that were reported by the various seismological institutions. In the most heavily damaged areas, 70–90% of units destroyed, contributing to a total of 4.1 million cubic meters of debris. Earthquake mitigation plan in the area has been carried out by understands the location of the fault. Merapi volcanic: did lahar deposits amplify ground shaking and thus lead to the disaster?," An Electronic Journal of the Earth Sciences, 9, 5 (2008). While some scientists have . This unconsolidated material from the stratovolcano amplified the intensity of the shaking and created the conditions for soil liquefaction to occur. The 2004 tsunami event triggered by a 9.1 magnitude earthquake in Sumatra, which killed over 200,000 people, has raised global awareness of tsunamis (Engel and Brückner 2011; Adyan 2008). 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. While volcanic activity and earthquakes are often connected, it is not clear if the May 27 earthquake is directly linked to Merapi’s activity, said the USGS. The Bantul-Klaten plain consists of alluvium (sand, silt, clay, and gravel) and volcanic deposits from Merapi (sand, agglomerates, tuff, and ash), as well as limestone and sandstone. Select Page. The 26 May 2006 teleseismic locations and focal mechanisms are provided by On 27 May 2006, an earthquake measuring 5.9 on the Richter scale struck Indonesia’s Java island. If the shock occurred in this area it could indicate the reactivation of a major fault system. 1. The USGS suggested that the focal mechanism was most likely associated with left-lateral slip on a NE trending strike-slip fault, as that is the orientation of the Opak Fault, but this has not been validated. The 2006 Yogyakarta earthquake (also known as the Bantul earthquake) occurred at .mw-parser-output .tooltip-dotted{border-bottom:1px dotted;cursor:help}05:54 local time on 27 May with a moment magnitude of 6.4 and a maximum MSK intensity of VIII (Damaging). NASA image created by Jesse Allen, Earth Observatory, using Shuttle Radar Topography Mission (SRTM) data provided courtesy of the Unviersity of Maryland’s Global Land Cover Facility. 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).Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3 . The quake destroyed more than 60,000 houses in the city, and killed an estimated 6,234 people, reported the World Health Organization on June 6. Earthquake fault of the 26 May 2006 Yogyakarta earthquake observed by SAR interferometry. This event also marks the 14th anniversary of the accident. Found inside – Page 51Syahirul Alim 5.1 Introduction Indonesia is located in the Pacific Ring of ... 5.2 The 2006 Yogyakarta and Central Java Earthquakes The 2006 Yogyakarta and ... Image of the Day Evidence for one of the proposed faults was found in the form of alignment of portions of the Oyo River near the USGS' epicenter, which is parallel (N°65E) to the Nglipar fault in the Gunungkidul region. The earthquake has also had a devastating effect of livelihoods, both as consequence of loss of production as families tend to their immediate shelter and emergency, but also because many people earned their living through ‘cottage’ industries, such as crafts and cooking. Magnitude: 6.3; Location: 7.962°S, 110.458°E) The theme raised in the disaster discussion this time was "The Reflection of Yogyakarta Earthquake 2006". One of the active fault in this region is the Opak fault which has striking south west - north east. In May 2006, the LDS Church donated $1.6 million USD worth of emergency supplies to devastated areas following the earthquake in Java, Indonesia, teaming up with Islamic Relief Worldwide who provided transportation in conjunction with The Islamic Medical Association of North America. Figure 1. Thousands of people perished, but many more s. This is an audio version of the Wikipedia Article: https://en.wikipedia.org/wiki/2006_Yogyakarta_earthquake 00:01:50 1 Tectonic setting 00:03:14 2 Earthquake. 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. Although Indonesia experiences very large, great, and giant thrust earthquakes offshore at the Sunda Trench, this was a large strike-slip event that occurred on the southern coast of Java near the city of Yogyakarta. due to its location . MERAPI Volcano This report is based on information received from the UN Resident . : 2007040289: Yogyakarta earthquake of May 27, 2006: data view (On May 27, 2006 a major earthquake occurred near Yogyakarta Indonesia -- the largest in 60 years! Applying lessons learned from the Aceh recovery from the 2004 Indian Ocean earthquake and tsunami, the government of Indonesia promoted a community-driven approach in reconstruction from the 2006 Yogyakarta earthquake. 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 . There were no direct effects of . 59 al. Location Semarang, Yogyakarta Shelter was needed for the homeless people, and many countries and organizations provided as- We welcome submissions, Yogyakarta and Central Java Earthquake, 2006, http://www.who.or.id/eng/php/content/jogja-centraljava/Sitrep%20Indonesia%20Jogja-Central%20Java%2004-06-06%20(7).pdf, Building on Success: Effectively Responding to Multiple Disasters, Early recovery and risk reduction - Yogyakarta & Central Java Earthquake, Supporting community recovery and risk reduction in Yogyakarta, Indonesia: Post-earthquake damage and loss assessment for Central Java and Yogyakarta, Recovery Status Report: The Yogyakarta and Central Java Earthquake 2006, © 2019 International Recovery Platform All rights reserved. Image of the Day We analyzed synthetic aperture radar interferometry (InSAR) to reveal surface deformation associated with the 26 May 2006 Yogyakarta earthquake, for which the fault location and geometry have not been clearly determined. (a) Location map. Aerial video was taken by from from the SAR helicopter. They're calling the event the Yogyakarta earthquake. No surface breaks were documented, but the location of the greatest . Many countries and organizations offered foreign aid to the devastated region, but the actual amounts delivered/received often varied from these figures, as in the case of other disasters. May 28, 2006. [23] stated that there are several versions of the location of the epicenter. Disaster Management and Human Health Risk II 55 WIT Transactions on the Built Environment, Vol 119, The Yogyakarta earthquake occurred on May 27, 2006, at 05:52 local time (or May 26, 2006, at 22:54 GMT) with its epicentre in the Indian Ocean at about 33 km south of the Bantul district in the Yogyakarta province (Bappenas 2006; see Fig. The Opak fault, a fault mapped by geologists was thought to be the source of this earthquake disaster. More than 2,000 residents of Bantul were killed, thousands of its residents injured, and 80% of its homes damaged or destroyed. 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. 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).Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3 . The unprecedented 26 May 2006 Yogyakarta earthquake (central Java, Indonesia) that took victims of 5,700 lives was generally accepted to have a depth of about 10 km and moment magnitude of 6.4. This paper focuses on the local economic growth impacts of a specific natural disaster, viz. Injured 58,790 Right: events after May 2006 - 2018. Earthquakes occur in the sometimes-messy grind of colliding plates, but these are centered deep below the Earth’s surface. [9], While the densely populated area that saw significant destruction is adjacent to the Opak River Fault, both the USGS and Harvard University placed the epicenter to the east of that fault. Merapi, an active volcano. In 2006, a large earthquake shocked the denselypopulated Yogyakarta Province and its surrounding areas. Low quality materials and improper construction styles led to unreinforced masonry buildings being responsible for the large loss of life and the high number of injuries. Indonesia 2006. They turned to traditional materials, such as bamboo, because of the damage inflicted by collapsing brick walls. Elnashai et al. A powerful earthquake rattled Yogyakarta, Java, Indonesia, in the early morning hours of May 27, 2006. Found inside – Page 10Major earthquakes that occurred in Java include the Banyuwangi earthquake in 1994, Yogyakarta, May 27, 2006 with epicenter 8.26°S - 110.31° E, magnitude 5.9 ... In the early hours of May 27, 2006, at approximately 05.54 local times, an earthquake struck the city of Yogyakarta. Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3 . We analyzed synthetic aperture radar interferometry (InSAR) to reveal surface deformation associated with the 26 May 2006 Yogyakarta earthquake, for which the fault location and geometry have not been clearly determined. no information present on extent of faulting or direction of propagation . Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3.1 billion). Found inside – Page 118This chapter makes an attempt to understand the determinants of micro, small and medium enterprise recovery after the 2006 Yogyakarta earthquake and the ... Left: events before May 2006 since 1971. May 27, 2006. socialization and on-the-spot training for the construction of earthquake-resistant housing such as penyuluhan and pelatihan teknis) and advocated for use of local materials (e.g., Merantasi). The location of the fault is still unclear among geoscientists until now. The image was created from data collected by the Shuttle Radar Topography Mission. The 2006 Yogyakarta earthquake was the second largest natural disaster after the earthquake and tsunami in Aceh which occurred in 2004. 63 Just a little memento of 2006 earthquake in Yogyakarta. Their investigation resulted in a different scenario, with an unknown or newly formed NE trending fault as the origin of the shock. The observed ground deformation that was detailed by the differential satellite images and Global Positioning System measurements was roughly 10 km (6.2 mi) east of (and parallel to) the Opak River Fault, along a zone that passed through the USGS' epicenter, and delineated a NE trending vertical fault (a dip of 89°). The information from the Agency for Meteorology, Climatology, and Geophysics of Indonesia (BMKG) showed it had a magnitude of Mw = 6.3, centered at 8.003E and 110.320 S with a depth of 11.87 km at the southeast of the city as shown in Fig. The Opak fault, a fault mapped by geologists was thought to be the source of this earthquake disaster. Found insidePeru's five-hundred-year earthquake: Vulnerability in historical context. ... Earthquake fault of the 26 May 2006 Yogyakarta earthquake observed by SAR ... Additionally, a 301 Moved Permanently error was encountered while trying to use an ErrorDocument to handle the request. Found inside – Page 28... Frozen yogurt industry Yogyakarta Earthquake , Indonesia , 2006 UF Java Earthquake , Indonesia , 2006 BT Earthquakes — Indonesia Yohimbine BT Rauwolfia ... Found inside – Page 97MAY 27th, 2006 Yogyakarta Earthquake on May 2006 was a strong tectonic ... the location of the earthquake was in coordinate 8,007° LS and 110,286° BT with ... 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).Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3 . For example, German and Indonesian scientists set up instruments at several locations situated on different soil types to measure aftershocks. The damage to housing accounted for about half of the total losses and a comparison was made to the damage to homes in Aceh following the 2004 Indian Ocean earthquake and tsunami. The volcano had been showing signs of increased activity since April, but activity picked up after the May 27 earthquake. The epicentre was located approximately 37 km south of the city of Yogyakarta. This image shows the topography of the landscape near the earthquake epicenter. On May 23, 2006 just before 6am, a 5.9 earthquake occurred some 20km south-southeast of Yogyakarta city. When the magnitude 6.3 earthquake struck at 5:54 a.m. on May 27, I was getting ready to go mountain biking up a beautiful hill southeast of Yogyakarta. Over 5,500 people were killed in the immediate aftermath . We analyzed synthetic aperture radar interferometry (InSAR) to reveal surface deformation associated with the 26 May 2006 Yogyakarta earthquake, for which the fault location and geometry have not been clearly determined, Our results demonstrate that surface deformation occurred ~10 km east of the Opak River fault thought to be the source of the May 2006 event and that the probable causative . . The earthquake impacted eight districts within Yogyakarta province and the neighbouring Central Java province, severely damaging housing and infrastructure. In this study, we analyzed aftershocks sequence through waveform data which taken from 16 temporary GeoForschungsZentrum (GFZ) network stasiuns located around the . Earthquake Information Center) indicates that the epicenter of the shock was at the south coast of Yogyakarta Province, south of Opak River with a Found inside – Page 47... The Case of the 2006 Yogyakarta Earthquake Mustika Septiyas Trisilia, ... such as earthquakes, volcanoes, and tsunamis due to its location on the Ring ... (b) Detailed map around Yogyakarta, with the epicenter of the 2006 Yogyakarta earthquake (yellow star) (USGS . The site, which has experienced about 16 earthquakes since the 9th-century (including the 2006 event), consists of three yards of varying sizes with different stone block temples, and was rediscovered by a Dutch explorer in 1733. (c) Shaded relief map of the Yogyakarta area, city center shown by white square symbol. No content reported. Yasuhiro Yamada. A unique interdisciplinary approach to disaster risk research, including global hazards and case-studies, for researchers, graduate students and professionals. Yogyakarta sits in a broad valley between two groups of roughly north-running mountains. [11], A separate post-event study looked at the relationship with the layer of sediment and the occurrence of soil liquefaction during earthquakes near Bantul. The May 27 earthquake happened near the surface along a fault in the Sunda Plate, about 20 kilometers south-southeast of Yogyakarta. Table 1 presents the earthquake details from the USGS report [2] for the event. Why 1964 Alaska earthquake and 2006 Yogyakarta earthquake are similar. Merapi activities was increasing. 1964 Alaska earthquake. [10], A lack of any dislocation found on the images along the Opak River fault made evident the lack of movement along that fault, and though the aftershocks were occurring at a depth of 8–15 km (5.0–9.3 mi), the deformation was distinct at the surface. Found inside – Page 267... involved 173 residents in Yogyakarta and 305 in Aceh conducted from December 2012—January 2013 or almost 6 years after 2006 Yogyakarta Earthquake and 8 ... 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).Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3 . [12], Altogether, eleven densely populated districts comprising 8.3 million people were affected, but the regencies of Bantul, Sleman, Gunung Kidul, Kulon Progo, Klaten, and the city of Yogyakarta were especially hard hit. Villagers rebuilt their homes with extremely limited resources, using simple affordable materials. The second proposed fault further to the east is nearly parallel to the Ngalang and Kembang faults that lie to the north of the Oyo River. 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). Found inside – Page 322The three cases include the decentralized approach of the IFRC to humanitarian logistics following the 2006 Indonesian earthquake in Yogyakarta, ... Yogyakarta earthquake, Mw 6.3, 27 May 2006 had killed 5,571 victims and destroyed more than 1 million buildings. 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