Earthquake & Tsunamis
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Dutch Donors Hand Over More Than 600 UN-HABITAT Houses on the Remote Island of Simeulue
United Nations Human Settlements Programme Programme des Nations Unies pour les établissements humains INDONESIA JL. T.M. Pahlawan No. 3A, Banda Aceh, Telephone : +62 651 25258 PRESS RELEASE Dutch donors hand over more than 600 UN-HABITAT houses on the remote island of Simeulue Sambai, Simeulue Island, Indonesia, 5 July – In a joyful ceremony in Sambai village on Simeulue Island UN-HABITAT, UNDP and the Aceh Rehabilitation and Reconstruction Agency celebrated the completion of houses together with Dutch donors and survivors of the Indian Ocean Tsunami. Daniel Biau (UN-HABITAT,right) and Simon Field (UNDP) plant a tree in front of a reconstructed house The director of the Regional and Technical Cooperation Division Nairobi, Daniel Biau, who visited Aceh Province to commemorate two years of UN-HABITAT’s and UNDP’s Aceh Nias Settlements Support Programme praised the successful collaboration work between UN- HABITAT, UNDP, the Aceh Nias Rehabilitation and Reconstruction Agency (BRR) and the people of Simeulue and their local authorities. The Aceh Nias Settlements Support Programme (ANSSP) has so far completed reconstruction of 3,500 houses and more than 1,000 are currently under construction in cooperation with the Asian Development Bank (ADB). In Simeulue, an island off the west coast of Sumatra, the recovery process has been particularly challenging. On the remote island the number of casualties was relatively small, because oral tradition had passed on the knowledge that people must run uphill after earthquakes to avoid tsunami waves. However, the destruction, which the disaster had left behind, was overwhelming. Whole villages had been wiped out. The shipment of material by sea and on the few bad roads was difficult and skilled workers were hard to find. -
Red Cross Red Crescent Looking Back, Moving Forward Issue 1
The future of international humanitarian law An artist’s view of the rules of war in the year 2064 Our Red Cross and Red Crescent stories 8 May theme celebrates your connection with the Movement Red Cross Red Crescent Looking back, moving forward Issue 1 . 2014 www.redcross.int Remembering Rwanda’s past and building a brighter future Programmed for war Imagining the future of armed confl ict THE MAGAZINE OF THE INTERNATIONAL RED CROSS AND RED CRESCENT MOVEMENT RCRC_1.14_Eng+_IRL.indd i 02.04.14 16:01 The International Red Cross and Red Crescent Movement is made up of the International Committee of the Red Cross (ICRC), the International Federation of Red Cross and Red Crescent Societies (IFRC) and the National Societies. International Federation of Red Cross and Red Crescent Societies The International Committee of the Red The International Federation of Red Cross National Red Cross and Red Crescent Societies Cross is an impartial, neutral and independent and Red Crescent Societies (IFRC) is the embody the work and principles of the organization whose exclusively humanitarian world’s largest volunteer-based humanitarian International Red Cross and Red Crescent mission is to protect the lives and dignity of network, reaching 150 million people each year Movement in more than 189 countries. National victims of armed confl ict and other situations of through its 189 member National Societies. Societies act as auxiliaries to the public authorities violence and to provide them with assistance. Together, the IFRC acts before, during and of their own countries in the humanitarian fi eld The ICRC also endeavours to prevent suff ering by after disasters and health emergencies to meet and provide a range of services including disaster promoting and strengthening humanitarian law the needs and improve the lives of vulnerable relief, health and social programmes. -
Fujinoetal-Margeo-Simeulue.Pdf
Marine Geology 357 (2014) 384–391 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Ambiguous correlation of precisely dated coral detritus with the tsunamis of 1861 and 1907 at Simeulue Island, Aceh Province, Indonesia Shigehiro Fujino a,⁎, Kerry Sieh b,1, Aron J. Meltzner b,1,EkoYuliantoc, Hong-Wei Chiang d,1 a Active Fault and Earthquake Research Center, National Institute of Advanced Industrial Science and Technology (AIST), Site C7 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan b Tectonics Observatory, California Institute of Technology, Pasadena, CA 91125, USA c Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung, Indonesia d High-precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan, ROC article info abstract Article history: Precise U–Th dates from coral detritus in two pre-2004 tsunami deposits on Simeulue Island in Aceh Province Received 7 March 2014 allow us to correlate the deposits with historically documented tsunamis in the recent few centuries, but because Received in revised form 19 September 2014 of potential discordance between the death dates of the corals and deposition of the sand layers, ambiguity in this Accepted 28 September 2014 correlation remains. Pits at coastal lowland sites exposed sand layers beneath the 2004 tsunami deposit at Available online 22 October 2014 Busung and Naibos on southern Simeulue Island. The layers share sedimentological characteristics with the de- Communicated by J.T. Wells posit of the 2004 tsunami, and are interpreted as pre-2004 tsunami deposits. Historical accounts document earth- quakes and tsunamis in 1907 and 1861 and suggest that the 1907 tsunami was larger locally than any others Keywords: historically. -
The Indian Ocean Tsunami: Economic Impact, Disaster Management and Lessons
The Indian Ocean Tsunami: Economic Impact, Disaster Management and Lessons Prema-chandra Athukorala and Budy P. Resosudarmo Division of Economics Research School of Pacific and Asian Studies Australian National University E-mail: [email protected] [email protected] Abstract: The purpose of this paper is to document and analyze the immediate economic impact of the Indian Ocean tsunami generated by the Sumatra-Andaman earthquake of 26 December 2004 and the disaster management process in the immediate aftermath of the disaster with a focus on the two worst affected countries – Indonesia (Aceh province) and Sri Lanka. The 26 December Tsunami is unique among large disasters in recorded human history, not only because of the sheer number of causalities and massive displacement of people, but also because of the unprecedented international donor response and the logistic challenges faced by international organizations and aid agencies in organizing and coordinating relief efforts. Our preliminary findings points to the importance of educating the public about simple precautions in the event of a disaster and enforcement of coastal environmental regulations as disaster prevention policies. The findings also makes a strong case for designing policies and programs, as an integral part of national development strategy, for mitigating the impact of natural disasters on the poor and highlights the need for combining international aid commitments with innovative approaches to redressing problems of limited aid absorptive capacity in disaster affected countries. Key Words: tsunami, disaster management, Indonesia, Sri Lanka JEL Classification: I32, O53 Q54 Forthcoming in Asian Economic Papers 1 2 The Indian Ocean Tsunami: Economic Impact, Disaster Management and Lessons∗ Sociologist, psychologists, historians, and policy planners have all devoted considerable attention to the nature, sources, and consequences of disaster and recovery, but the professional economic literature is distressingly sparse. -
Mental Health Matters: Mapping of Mental Health and Psychosocial Support Activities Within the International Red Cross and Red Crescent Movement
Mental Health Matters: Mapping of Mental Health and Psychosocial Support Activities within the International Red Cross and Red Crescent Movement December 2019 1 Executive summary The International Red Cross and Red Crescent Movement Project on Addressing 74% (120 NS, the IFRC and the ICRC) have one or more focal points for MH Mental Health and Psychosocial Consequences of Armed Conflicts, Natural Disas- and/or PSS in their organization. Collectively, within the 162 NS respondents, ters and other Emergencies (MOMENT) has conducted a survey to establish a da- IFRC and ICRC, nearly 27.000 staff and volunteers are reported to be trained in taset and baseline for mental health and psychosocial support (MHPSS) activities basic community-based psychosocial support, and more than 42.000 staff and carried out by the Movement. A total of 162 National Societies (NS), the Interna- volunteers are trained in PFA within the 162 NS and IFRC. Further, 77% (125 NS, tional Federation of the Red Cross and Red Crescent Societies (IFRC) and the In- the IFRC and the ICRC) have some sort of system in place to monitor the MH ternational Committee of the Red Cross (ICRC) participated. This report contains and/or PSS activities of their organization. the results of the survey. 34% of respondents (55 NS) have no budget dedicated for MHPSS activities, and 96% of respondents (156 NS, the IFRC and ICRC) provide mental health (MH) 83% (135 NS and the IFRC report that lack of or limited funds is an obstacle for and/or psychosocial support (PSS) activities. In the past year psychological first delivering MH and/or PSS activities. -
Draft GHI Guide
Preparing Your Community for Tsunamis A Guidebook for Local Advocates page 1 GHI Tsunami Guidebook, DRAFT April 5 2007 Simeulue Island: Local Knowledge Saves Lives On December 26, 2004 a tsunami, caused by a large earthquake under the sea off of Indonesia, spread throughout the Indian Ocean. It killed over 230,000 people in Indonesia, Thailand, India, Sri Lanka and elsewhere and destroyed the homes and livelihoods of many more. That day Simeulue Island, Indonesia was one of the many places inundated with the tsunami’s destructive waves. But the tsunami’s impact in Simuelue Island was not like what happened in other places: only seven people were killed by the tsunami in Simeulue out of a population of nearly 80,000. Why? Because the island’s residents had passed down stories about earlier tsunamis to strike the island, warning people to head to high ground if they felt strong earthquake shaking. These stories were known to most island residents from childhood. And on December 26, people on the island followed the guidance of these stories and saved their lives. The earthquake that triggered the 2004 mega-tsunami was centered only 40 kilometers away from the northern part of Simeulue. The first tsunami waves struck the northern coast of the island about ten minutes after the earthquake and caused widespread damage to buildings, which had already been evacuated. In 2004, no official tsunami warning system was in place for Simeulue, or any other part of the Indian Ocean. But even if one had existed, it would have been unlikely to warn the island’s residents quickly enough to evacuate people before the first waves struck. -
Postseismic Slip Following the 2005 Nias-Simeulue, Sumatran Indonesia Earthquake
Postseismic slip following the 2005 Nias-Simeulue, Sumatran Indonesia earthquake Ya-Ju Hsu1, Mark Simons1, Jean-Philippe Avouac1, Kerry Sieh1, John Galetzka1, Yehuda Bock2, Danny Natawidjaja3 and Linette Prawirodirdjo2 1. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. 2. Institute of Geophysics and Planetary Physics, University of California San Diego, California, U.S.A. 3. Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung, Indonesia. Abstract The March 28, 2005 Nias-Simeulue Mw 8.7 earthquake ruptured the plate boundary megathrust on the northwest coast of Sumatra, southeast of the December 26, 2004 Mw 9.1 Aceh-Andaman earthquake. The availability of 3-component continuous GPS data and microatoll observations of vertical displacements for this event, all located above or near the region of coseismic rupture, permits us to address a disparate suite of questions regarding the mechanical nature of the megathrust. For the first time, we unambiguously determine that significant post-seismic slip occurred updip from the coseismic rupture, consistent with the notion that the shallow-most portions of the subduction interface primarily slips aseismically. Generally, the regions of major coseismic and postseismic slip are mutually exclusive and after 9 months many portions of the megathrust are still slipping at rates several times the long-term average interseismic rate. The observed relationship between the spatial and temporal evolution of cumulative postseismic displacement and the cumulative number of aftershocks is consistent with a model in which the location and number of aftershocks is driven by induced afterslip and not directly by coseismic stress changes. -
Sibling Earthquakes Generated Within a Persistent Rupture Barrier on the Sunda Megathrust Under Simeulue Island
Geophysical Research Letters RESEARCH LETTER Sibling earthquakes generated within a persistent 10.1002/2016GL071901 rupture barrier on the Sunda megathrust Key Points: under Simeulue Island • The 2002 Mw 7.3 and 2008 Mw 7.4 Simeulue earthquakes are “sibling” 1 1 1 1 1 earthquakes that resemble each Paul M. Morgan , Lujia Feng , Aron J. Meltzner , Eric O. Lindsey , Louisa L. H. Tsang , other and largely overlap and Emma M. Hill1,2 • These two ruptures slipped an isolated, locked asperity within a 1Earth Observatory of Singapore, Nanyang Technological University, Singapore, 2Asian School of the Environment, persistent rupture barrier to great Nanyang Technological University, Singapore earthquakes • The rupture terminations and seismic asperity under Simeulue may be structurally controlled by Abstract A section of the Sunda megathrust underneath Simeulue is known to persistently halt a subducting morphological high rupture propagation of great earthquakes, including those in 2004 (Mw 9.2) and 2005 (Mw 8.6). Yet the of the slab same section generated large earthquakes in 2002 (Mw 7.3) and 2008 (Mw 7.4). To date, few studies have investigated the 2002 and 2008 events, and none have satisfactorily located or explained them. Using Supporting Information: near-field InSAR, GPS, and coral geodetic data, we find that the slip distributions of the two events are • Supporting Information S1 not identical but do show a close resemblance and largely overlap. We thus consider these earthquakes •DataSetS1 •DataSetS2 “siblings” that were generated by an anomalous “parent” feature of the megathrust. We suggest that •DataSetS3 this parent feature is a locked asperity surrounded by the otherwise partially creeping Simeulue section, •DataSetS4 perhaps structurally controlled by a broad morphological high on the megathrust. -
Danish Red Cross COVID-19 Preparedness Profile(As of May 5
Danish Red Cross COVID-19 preparedness profile (as of May 5, 2020) Risk & Hazards Pre-hospital care: Yes 1 INFORM COVID-19 Risk Index Health Centre(s): - Hazard & Lack coping Hospital(s): - Vulnerability Risk class Exposure capacity Higher Education: - 2.9 7.1 0.2 Low INFORM COVID-19 risk rank: 183 of 191 countries Programmes Highlighted INFORM COVID-19 sub-components Community-based Health & First Aid (CBHFA)17 Socio-Economic Vulnerability: 0.2 Is CBHFA active: Food Security: 1.4 Yes No CBHFA activities: Gender Based Violence (GBV): 0.7 - Movement (international & national): 8.8 No Health topics taught: - Behaviour (awareness & trust)): 2.7 Community Engagement & Accountability (CEA)18 Governance (effectiveness & corruption): 1.3 Access to healthcare: 1.1 HR Capacity: 3-Day Training/ToT Health context Structure: - Global Health Security Index:2 8 out of 195 No Programs: Global Health Security preparedness levels: - 14 Preventing pathogens: Most prepared Mental Health and Psychosocial Support (MHPSS) Early detection/reporting of epidemics: Most prepared Number of volunteers trained in: Basic Psychosocial support (PSS): 1,000 Responding & mitigating spread: More prepared Psychological First Aid (PFA): 1,000 Treat the sick & protect health workers: More prepared Number of highly skilled volunteers: Social Workers (0), Psychologist (0), Psychiatrist (0), Community Healthcare Commitments (HR, funding & norms): More prepared Workers (CHWs) (0) Risk/vulnerability to biological threats: Least at risk 29 current Psychosocial (PSS) activities: Restoring -
The Northern Sumatra Earthquake of March 28, 2005
EERI Special Earthquake Report — August 2005 Learning from Earthquakes The Northern Sumatra Earthquake of March 28, 2005 Editor’s Note: Beginning with the killed around 1,000 people while they occurred. Right after the earth- March issue and in each one sub- were either sleeping or trying to run quake, electric power was cut off sequently, we presented six reports from the second and third fl oors. In and telecommunication disrupted. by the many teams that observed Simeulue, some house shops col- In Gunung Sitoli and Teluk Dalam, the effects of the December 26, lapsed, and about 100 people were Nias, the damage was concentrated 2004, earthquake and tsunami in killed. There was a rush to exit in certain areas close to the beach. countries around the Indian Ocean. houses and run to higher places be- In Simeulue the damage was also This report adds information on cause the people feared a tsunami concentrated in areas close to the structural damage, largely from similar to that of December 26, 2004. beach. Strong aftershocks (32 km shaking, on two islands west of There was a local tsunami, but not from Gunung Sitoli [M 6.0] and 41 Sumatra in a subsequent large of the size or ferocity of the previous km from Sinabang (M 5.5]) did not earthquake in roughly the same one. cause any further damage to either epicentral area as the December damaged or undamaged buildings. quake. Publication of this report is Nias Island is part of North Sumatra supported by funds from the Na- Province and Simeulue Island is part tional Science Foundation through of Aceh Province. -
Reinventing Tradition: New Dance in Indonesia 1 by Sal Murgiyanto
Reinventing Tradition: New Dance in Indonesia 1 by Sal Murgiyanto Introduction I would like to begin this lecture by expressing my sincerest respect and deepest sorrow for the thousands of people who died as victims of the dreadful earthquake and deadly tsunami in Sri Lanka, India, Thailand, and Aceh, Indonesia. Still, in the midst of the disturbing pictures and reports published in newspapers, and eerie scenes broadcast on television in December 2004, miracles were also told. A two month-old baby girl was sucked into an undertow and thrown back by a tidal wave alive into her mother’s lap. Early in the morning after Christmas, a ten-year-old girl sat beside her father enjoying the beauty of Phuket’s beach in Thailand. Upon seeing the water on the beach receding drastically and, from afar, white tidal waves surging one after the other, Kelly told her dad, “A tsunami is coming in twenty or thirty minutes and there will be disaster!” She had learned this fact in a class prior to her vacation. The wise father told the story to a coastguard who ordered everybody to leave the beach immediately and head back to the hotel. This speedy action saved more than 400 human lives; thirty minutes after the announcement the tsunami destroyed everything standing on the beach. Saving the lives of many, Kelly was called the “Angel of [the] Beach.” 2 There is still one more miracle to relate. Forty kilometers from the epicenter of the December 2004 earthquake sits Simeulue, a small island in the Indian Ocean 150 kilometers off the west coast of the province of Aceh, on the island of Sumatra in Indonesia. -
Rupture and Variable Coupling Behavior of the Mentawai Segment of the Sunda Megathrust During the Supercycle Culmination of 1797
PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Ruptureandvariablecouplingbehavior 10.1002/2014JB011200 of the Mentawai segment of the Sunda Key Points: megathrust during the supercycle • The 1797/1833 Mentawai earthquakes were much larger than the culmination of 1797 to 1833 2007 earthquakes • The interseismic coupling pattern Belle Philibosian1,2, Kerry Sieh3, Jean-Philippe Avouac1, Danny H. Natawidjaja4, Hong-Wei Chiang5,6, fi changed signi cantly after 1797 5 1,7 5 8 • Heterogeneity of frictional properties Chung-Che Wu , Hugo Perfettini , Chuan-Chou Shen , Mudrik R. Daryono , 4 may cause the “supercycle” behavior and Bambang W. Suwargadi 1Tectonics Observatory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, Supporting Information: California, USA, 2Now at Équipe de Tectonique et Mécanique de la Lithosphère, Institut de Physique du Globe de Paris, Paris, • Readme 3 4 • Table S1 and Figures S1–S37 France, Earth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore, Research Center for Geotechnology, Indonesian Institute of Science (LIPI), Kampus LIPI Bandung, Bandung, Indonesia, 5High-Precision Mass Correspondence to: Spectrometry and Environment Change Laboratory, Department of Geosciences, National Taiwan University, Taipei, Taiwan, B. Philibosian, 6Now at the Earth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore, 7Now at IRD/ISTerre, [email protected] Université Joseph Fourier, Grenoble, France, 8Institut Teknologi Bandung, Bandung, Indonesia Citation: We refer to periods of subduction strain accumulation beneath the Mentawai Islands, Sumatra, Philibosian, B., K. Sieh, J.-P. Avouac, Abstract D. H. Natawidjaja, H.-W. Chiang, C.-C. Wu, as “supercycles,” because each culminates in a series of partial ruptures of the megathrust in its final decades.