Historical Study of Tsunamis - an Outline

Total Page:16

File Type:pdf, Size:1020Kb

Historical Study of Tsunamis - an Outline Pacific Marine Science Report 78-5 HISTORICAL STUDY OF TSUNAMIS - AN OUTLINE by Sydney O. Wigen Institute of Ocean Sciences, Patricia Bay Sidney, B.C. Pacific Marine Science Report 78-5 HISTORICAL STUDY OF TSUNAMIS - AN OUTLINE by Sydney O. Wigen Institute of Ocean Sciences, Patricia Bay Sidney, B.C. January 1978 This is a manuscript which has received only limited circulation. On citing this report in a bibliography, the title should be followed by the words "UNPUBLISHED MANUSCRIPT" which is in accordance with accepted bibliographic custom. ..I ABSTRACT This paper is intended to set forth objectives for a Historical Study of Tsunamis; to summarize the preparatory work carried out at the International Tsunami Information Center; and to provide a procedural outline for those participating in the Study. From Basi1an Island, Philippines August 1976 "When the tsunami broke down our homes our people tried to go to higher ground. If the water was above our knees a man could hardly stand, and women and children did not have a chance". HISTORICAL STUDY OF TSUNAMIS - AN OUTLINE Letter of Introduction During the final months of his posting as Associate Director of the International Tsunami Information Center, Mr. Sydney o. Wigen has undertaken preparatory work on behalf of ITIC for a comprehensive Historical Study of Tsunamis. The Center endorses this Study, and authorizes Mr. Wigen to continue to co-ordinate and direct it on behalf of the Center. Bringing the Historical Study of Tsunamis to a success­ ful fulfillment will only be possible with the co-operative participation of many researchers. From it may come a syste­ matic body of knowledge that could be applied to mitigating the effects of tsunamis, and protection of people and property in coastal communities throughout the world. Mr. Wigen is completing his posting as Associate Director of ITIC on November 30, 1977 and is returning to Canada where he is continuing in tsunami programs. Questions, comments and expressions of interest in participating in the Historical Study of Tsunamis may be sent to ITIC, or directly to Mr. Wigen at his new address; Institute of Ocean Sciences; P.O. Box 6000; 9860 W. Saanich Road; Sidney, B.C., Canada; V8L 4B2. Sincerely, George Pararas-Carayannis Director, ITIC 1 HISTORICAL STUDY OF TSUNAMIS - AN OUTLINE This paper is intended to set forth objectives for a Historical Study of Tsunamis; to summarize the preparatory work carried out at the International Tsunami Information Center; and to provide a procedural outline for those participating in the Study. Introduction In a recent study by the author, the marigrams from the tide station at Tofino, British Columbia, were examined for evidence of 70 known large tsunamis originating in various parts of the Pacific. Twenty-one of these were found to have produced identifiable tsunamis, and most of these had not been previously reported. It was recognized that many additional.tsunamis could have reached and been recorded at Tofino, and that these could be uncovered by a systematic search of a large number of potentially tsunamigenic events. Similarly, a study of the marigrams from any other tidal station would yield an unknown number of previously unreported tsunami records. A systematic search through tide records of many stations and the compiling of standardized data would provide a foundation for tsunami research that would have direct application for the improvement of tsunami warning systems. with this in mind, preparatory work for a systematic and com­ prehensive Historical Study of Tsunamis has been carried out at the International Tsunami Information Center, and is outlined in this paper. The full Study can be brought to successful fulfillment with the co-operation of many researchers, each investigating the tsunami records from a single tidal station. It is envisaged that each of the research studies will provide a body of knowledge not presently available, and the composite of many such studies will be a data source for ocean-wide research. 2 9b jectives About 100,000 people are known to have died as a result of tsunamis in the last 100 years, the period of time to be covered by this Study. Most died for lack of knowledge and preparedness. Researchers may recognize in the following statement of objectives, the potential of the Study to mitigate some of the disastrous effects of tsunamis, and how their own participation will add to the body of knowledge, assist in the development of regional and International Tsunami Warning Systems, and contribute to the protection of property and resources and the saving of lives. Here are the principal objectives, as related to each specific station. 1. Identify whether the coastal area at which the station is located is vulnerable to destructive tsunamis, and establish the frequency with which tsunamis of any magnitude may be expected. 2. Define which tsunami-generating regions threaten the coastal area, and which do not. 3. Determine the actual travel times of tsunamis from generating regions, and the number of hours after arrival that the waves may have their maximum impact. 4. Evaluate how accurately the gauge station records tsunamis affecting the adjacent coast, and determine whether its capability could be improved. Here are the principal objectives, related to the collective results of the Historical Study of Tsunamis. 3 1. Collect and systematize as complete a record as possible of tsunamis, and standardize data, as a foundation for research. 2. Identify the directions in which generated tsunamis propagated; find whether the direction of propagation from any source was consistent; and define the directions in which each did not propagate. 3. Develop a body of data on actual travel times of tsunamis, for use in calibrating travel time charts used in warning systems. 4. Provide data for calibrating numerical models of tsunamis in the ocean. 5. Identify earthquakes that produced tsunamis, and ones of similar magnitude that apparently did not. Characteristics of their seismic records may be recognized that could identify the tsunami threat of future earthquakes at the time of their occurrence. The collected data from the Historical Study of Tsunamis will be provided to the World Data Centers for Tsunamis. In this way any researcher will have access to it for further investigation. Preparatory Work The basic procedure adopted for the Study has been to compile a list of earthquakes whose magnitude, depth, and location would make them potentially tsunamigenic; to supplement these events with other known or suspected tsuanmis; and t9 define stann~rdiz­ ed procedures for data collection and compilation. Tsunami' catalogues by Iida, Cox~ and Pararas-Carayannis, 1967 and by Soloviev, 1974 and 1975, provided most of the records of past tsunamis, and these were supplemented by records of the Honolulu 4 Observatory (now the PaciIic Tsunami Warning Center), and by a number of papers dealing with specific regions. A paper by S. J. Duda, and pUblications of the International Seismological Centre and the National Earthquake Information Service were the primary sources of earthquake data. Regional data were received as well from New Zealand and from Canada. The preparation of the list of potentially tsunamigenic events required a number of arbitrary judgements, so the procedures for selection are outlined below. Arbitrarily the list commences in 1883, the year of the Krakatoa explosion and tsunami. For the first 14 years, 1883-1896, adequate earthquake records do not appear to be available, and only 18 events were selected from the tsunami catalogues. For the period 1897-1964, the list of earthquakes compiled by S. J. Duda was recommended by seismologists as being the most reliable. This list included all earthquakes of magnitude 7.0 and larger, about 1300 in all for the 68 years. From these were deleted earthquakes that appeared to be too far inland to be tsunamigenic, and those with a focal depth of greater than 100 km. Events from tsunami catalogues were added, resulting in about 1020 events for the 68 years. In setting criteria to keep the Study to a manageable size and delete earthquakes most unlikely to be tsunamigenic, a few actual tsunamis will have been missed. In four cases the tsunami catalogues restored events that had been deleted from the earthquake list because of focal depth. From 1965 through 1974 the semiannual list of large earthquakes published by the International Seismological Centre (ISC) was used. Each edition includes a list of major earthquakes, magnitude 5.5 and over. The ISC magnitude is given, plus magnitudes established by other sources for the same event. Typically 5 there is a disparity of .5 to 1.0 in the magnitudes, with ISC and United states Coast and Geodetic Survey (USCGS) 1965-1970, or National Earthquake Information Service (NElS) 1971-1974 being low, but in close agreement, and others being relatively high. By comparison with events in the tsunami catalogues it appeared appropriate to select earthquakes with an ISC or NElS magnitude of 6.0 or larger, and about 400 events were included for this 10 year period. For 1975 and 1976 the principal source of information was the record of earthquakes investigated by Honolulu Observatory, and 50 events were included. For all of the above periods the NElS catalogue of earthquakes was a valuable corroborative data -source, particularly when times and positions from other records were in disagreement. The list of events has been prepared in two forms, a Chronological List and an Area List. Examples appear as Tables 1 and 2. The Chronological List defines the events, in time sequence. The Area List provides a form for tabulating standard information about any tsunami from these events, as recorded at a particular tide gauge station. In the Chronological List, the following abbreviations are used to designate principal data source for each event: TC Preliminary Catalogue of Tsunamis in the Pacific NG Science in New Guinea 4(1) 1976 DU S.
Recommended publications
  • Historical and Paleo-Tsunami Deposits During the Last 4000 Years and Their
    Ishimura and Miyauchi Progress in Earth and Planetary Science (2015) 2:16 DOI 10.1186/s40645-015-0047-4 RESEARCH ARTICLE Open Access Historical and paleo-tsunami deposits during the last 4000 years and their correlations with historical tsunami events in Koyadori on the Sanriku Coast, northeastern Japan Daisuke Ishimura1* and Takahiro Miyauchi2 Abstract Large tsunamis occurring throughout the past several hundred years along the Sanriku Coast on the Pacific coast of northeastern Japan have been documented and observed. However, the risk of large tsunamis like the tsunami generated by the 2011 off the Pacific coast of Tohoku earthquake could not be evaluated from previous studies, because these studies lacked evidence of historical and paleo-tsunami deposits on the coastline. Thus, we first identified event deposits, which are candidates for tsunami deposits, from excavating surveys conducted on the coastal marsh in Koyadori on the Sanriku Coast, northeastern Japan. Second, we determined the physicochemical sediment properties of the deposits (roundness of grains, color, wet and dry densities, and loss on ignition) and established their geochronology by radiocarbon dating and tephra analysis. Third, we identified event deposits as tsunami deposits, based on their sedimentary features and origin, sedimentary environment, paleo-shoreline, and landowner interviews. In this study, we report 11 tsunami deposits (E1–E11) during the past 4000 years, of which E1, E2, E3, and E4 were correlated with the 2011 Tohoku-oki tsunami, the 1896 Meiji Sanriku tsunami, the 1611 Keicho Sanriku tsunami, and the 869 Jogan tsunami, respectively. From age data and the number of tsunami deposits in the trench, we estimated that tsunamis larger than the 1896 Meiji Sanriku tsunami occur and hit the study area on average every 290–390 years.
    [Show full text]
  • TSUNAMIGENIC SOURCES in the INDIAN OCEAN R. K. Jaiswal , B. K
    TSUNAMIGENIC SOURCES IN THE INDIAN OCEAN 1 1 2 R. K. Jaiswal , B. K. Rastogi & Tad S. Murty 1 Institute of Seismological Research, Gandhinagar-382 018, Gujarat (India) 2 University of Ottawa, Ottawa, Canada Email: [email protected] ABSTRACT Based on an assessment of the repeat periods of great earthquakes from past seismicity, convergence rates and paleoseismological results, possible future source zones of tsunami generating earthquakes in the Indian Ocean (possible seismic gap areas) are identified along subduction zones and zones of compression. Central Sumatra, Java, Makran coast, Indus Delta, Kutch-Saurashtra, Bangladesh and southern Myanmar are identified as possible source zones of earthquakes in near future which might cause tsunamis in the Indian Ocean, and in particular, that could affect India. The Sunda Arc (covering Sumatra and Java) subduction zone, situated on the eastern side of the Indian Ocean, is one of the most active plate margins in the world that generates frequent great earthquakes, volcanic eruptions and tsunamis. The Andaman- Nicobar group of islands is also a seismically active zone that generates frequent earthquakes. However, northern Sumatra and Andaman-Nicobar regions are assessed to be probably free from great earthquakes (M!8.0) for a few decades due to occurrence of 2004 Mw 9.3 and 2005 Mw 8.7 earthquakes. The Krakatau volcanic eruptions have caused large tsunamis in the past. This volcano and a few others situated on the ocean bed can cause large tsunamis in the future. List of past tsunamis generated due to earthquakes/volcanic eruptions that affected the Indian region and vicinity in the Indian Ocean are also presented.
    [Show full text]
  • Boris W. Levin · Mikhail A
    Boris W. Levin · Mikhail A. Nosov Physics of Tsunamis Second Edition Physics of Tsunamis Boris W. Levin • Mikhail A. Nosov Physics of Tsunamis Second Edition 123 Boris W. Levin Mikhail A. Nosov Russian Academy of Sciences Faculty of Physics Yuzhno-Sakhalinsk M.V. Lomonosov Moscow State University Russia Moscow Russia ISBN 978-3-319-24035-0 ISBN 978-3-319-24037-4 (eBook) DOI 10.1007/978-3-319-24037-4 Library of Congress Control Number: 2015949315 Springer Cham Heidelberg New York Dordrecht London © Springer International Publishing Switzerland 2009, 2016 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. The publisher, the authors and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made.
    [Show full text]
  • The 1867 Virgin Island Tsunami
    Natural Hazards and Earth System Sciences (2003) 3: 367–376 c European Geosciences Union 2003 Natural Hazards and Earth System Sciences The 1867 Virgin Island Tsunami N. Zahibo1, E. Pelinovsky2, A. C. Yalciner3, A. Kurkin4, A. Koselkov4, and A. Zaitsev4 1Laboratoire de Physique Atmospherique´ et Tropicale, Departement´ de Physique , Universite´ Antilles Guyane, Pointe-a-Pitre, France 2Laboratory of Hydrophysics and Nonlinear Acoustics, Institute of Applied Physics, Nizhny, Novgorod, Russia 3Civil Engineering Department, Ocean Engineering Research Center, Middle East Technical University, Ankara, Turkey 4Applied Mathematics Department, Nizhny Novgorod State Technical University, Nizhny Novgorod, Russia Received: 7 October 2002 – Revised: 5 February 2003 – Accepted: 7 February 2003 Abstract. The 1867 Virgin Island Tsunami reached large catastrophic tsunamis are not well documented and cannot magnitude on the coasts of the Caribbean Islands. A max- be confirmed as true tsunamis. On the basis of these data, imum tsunami height of 10 m was reported for two coastal a rough evaluation of the cumulative frequency of tsunamis locations (Deshaies and Sainte-Rose) in Guadeloupe. Mod- was done for Barbados and Antigua (Zahibo and Pelinovsky, elling of the 1867 tsunami is performed in the framework 2001). The accuracy of such estimates is low, and numer- of the nonlinear shallow-water theory. The directivity of ical simulation of the historical and prognostic tsunamis is the tsunami wave source in the Caribbean Sea according to necessary to create a more reliable tsunami database. In the assumed initial waveform is investigated. The tsunami particular, tsunamis can be generated by volcanic eruptions. records at the several coastal regions in the Lesser Antilles, The Soufriere Hills Volcano in Montserrat erupted several Virgin Islands, Puerto Rico and South America are simu- times in the 90s (Hooper and Mattioli, 2001) and gener- lated.
    [Show full text]
  • Long-Term Perspectives on Giant Earthquakes and Tsunamis at Subduction Zones∗
    ANRV309-EA35-12 ARI 20 March 2007 15:19 Long-Term Perspectives on Giant Earthquakes and Tsunamis at Subduction Zones∗ Kenji Satake1 and Brian F. Atwater2 1Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, Tsukuba, 305-8567, Japan; email: [email protected] 2U.S. Geological Survey at University of Washington, Seattle, Washington 98195-1310; email: [email protected] Annu. Rev. Earth Planet. Sci. 2007. 35:349–74 Key Words First published online as a Review in Advance on paleoseismology, earthquake recurrence, earthquake forecasting, January 17, 2007 Sumatra, Chile, Cascadia, Hokkaido The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract by Brian Atwater on 05/14/07. For personal use only. This article’s doi: Histories of earthquakes and tsunamis, inferred from geological ev- 10.1146/annurev.earth.35.031306.140302 idence, aid in anticipating future catastrophes. This natural warn- Copyright c 2007 by Annual Reviews. ! ing system now influences building codes and tsunami planning in All rights reserved the United States, Canada, and Japan, particularly where geology 0084-6597/07/0530-0349$20.00 demonstrates the past occurrence of earthquakes and tsunamis larger Annu. Rev. Earth Planet. Sci. 2007.35:349-374. Downloaded from arjournals.annualreviews.org ∗The U.S. Government has the right to retain a than those known from written and instrumental records. Under fa- nonexclusive, royalty-free license in and to any vorable circumstances, paleoseismology can thus provide long-term copyright covering this paper. advisories of unusually large tsunamis. The extraordinary Indian Ocean tsunami of 2004 resulted from a fault rupture more than 1000 km in length that included and dwarfed fault patches that had broken historically during lesser shocks.
    [Show full text]
  • Tsunami History - Recorded
    TSUNAMI HISTORY - RECORDED V.K.Gusiakov Tsunami Laboratory, Institute of Computational Mathematics and Mathematical Geophysics, Siberian Division, Russian Academy of Sciences, Pr.Lavrentieva, 6, Novosibirsk 630090, Russia, Email: [email protected] Introduction Historical data on tsunami occurrence and coastal run-up are important for basic understanding of the tsunami phenomenon, its generation, propagation and run-up processes, its damaging effects. Such data are widely used for evaluating tsunami potential of coastal areas and for determining of the degree of tsunami hazard and risk for use in coastal-zone management and disaster preparedness. Also, historical data are of a critical importance for real-time evaluation of underwater earthquakes by the operational Tsunami Warning Centers, for the establishment of thresholds for issuing tsunami warnings and for design criteria for any tsunami-protective engineering construction. In terms of documented total damage and loss of human lives, tsunamis do not come first among other natural hazards. With an estimated 700,000 fatalities, resulted from tsunamis for all historical times (Gusiakov et al., 2007), they rank fifth after earthquakes, floods, typhoons and volcanic eruptions. However, because they can affect densely populated and usually well- developed coastal areas, tsunamis can have an extremely adverse impact on the socioeconomic infrastructure of society, which is strengthened by their full suddenness, terrifying rapidity, and their potential for heavy destruction of property and high percentage of fatalities among the population exposed to their action. There is evidence that tsunami as a catastrophic natural phenomenon has been known by humankind since antiquenty. Many languages have of a special word for this type of disaster coming from the sea - tidal waves, seismic sea waves (English), raz de maree, vagues sismiques (French), flutwellen (German), maremoto (Spanish), vlogengolden (Holland), tsunami (Japanese), hai-i Chinese, loka (Fijian).
    [Show full text]
  • Tsunamis Observed on and Near the Turkish Coast
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/226113643 Tsunamis Observed on and Near the Turkish Coast Article in Natural Hazards · January 2000 DOI: 10.1023/A:1008155117243 CITATIONS READS 91 453 2 authors: Yıldız Altınok Şükrü Ersoy Istanbul University Yildiz Technical University 64 PUBLICATIONS 834 CITATIONS 64 PUBLICATIONS 544 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: TRANSFER View project Acil saha gözlem View project All content following this page was uploaded by Şükrü Ersoy on 08 November 2014. The user has requested enhancement of the downloaded file. Natural Hazards 21: 185–205, 2000. 185 © 2000 Kluwer Academic Publishers. Printed in the Netherlands. Tsunamis Observed on and Near the Turkish Coast Y. ALTINOK1 andS. ¸ ERSOY2 1Department of Geophysical Engineering, Faculty of Engineering, University of Istanbul, 34850 Avcilar, Istanbul, Turkey; 2Department of Geological Engineering, Faculty of Engineering, University of Istanbul, 34850 Avcilar, Istanbul, Turkey (Received: 21 July 1998; in final form: 6 December 1999) Abstract. For centuries, inhabitants of coastal areas have suffered from the effects of tsunamis. Turkey, with a coastline of 8333 km, has experienced many tsunamis. Historical records reveal that, during the observation period over 3000 years, the coastal and surrounding areas of Turkey have been affected by more than ninety tsunamis. These tended to cluster around the Marmara Sea, the city of Istanbul and the gulfs of Izmit, Izmir, Fethiye and Iskenderun. Each of the tsunami occurrences surveyed in this paper deserves further individual study. The most extensive available information concerns the tsunamis associated with the Istanbul Earthquakes of 1509 and 1894, the Eastern Mar- mara Earthquake in 1963 and that of Izmit in 1999, which disturbed the Marmara Sea; the Earthquake of 1939 in Erzincan in eastern Anatolia; and the 1968 Bartın Earthquake, which affected Fatsa and Amasra on the Black Sea.
    [Show full text]
  • Tsunami Information Sources
    UC Berkeley Hydraulic Engineering Laboratory Reports Title Tsunami Information Sources Permalink https://escholarship.org/uc/item/4xk8j05g Author Wiegel, Robert L Publication Date 2005-12-14 eScholarship.org Powered by the California Digital Library University of California University of California, Berkeley, California 94720 Department of Civil & Environmental Engineering Hydraulic Engineering Laboratory Technical Report UCB/HEL 2005-1 TSUNAMI INFORMATION SOURCES By Robert L. Wiegel, Professor Emeritus Dept. Civil & Environmental Engineering 410 O'Brien Hall, MC 1718 University of California Berkeley, California 94720-1718 14 December 2005 University of California, Berkeley, California 94720 Department of Civil & Environmental Engineering Hydraulic Engineering Laboratory, Report UCB/HEL 2005-1 14 December 2005 TSUNAMI INFORMATION SOURCES By Robert L. Wiegel, Professor Emeritus Dept. Civil & Environmental Engineering 410 O'Brien Hall, MC 1718 University of California Berkeley, California 94720-1718 INTRODUCTION I have expanded substantially my list of information sources on: tsunami generation (sources, impulsive mechanisms), propagation, effects of nearshore bathymetry, and wave run-up on shore - including physical (hydraulic) modeling and numerical modeling. This expanded list includes the subjects of field investigations of tsunamis soon after an event; damage effects in harbors on boats, ships, and facilities; tsunami wave-induced forces; damage by tsunami waves to structures on shore; scour/erosion; hazard mitigation; land use planning;
    [Show full text]
  • Tsunami Hazard Evaluation of the Eastern Mediterranean: Historical Analysis and Selected Modeling by Amos Salamon, Thomas Rockwell, Steven N
    Name /mea_ssa973_605415/973_06147/Mp_1 04/04/2007 12:51PM Plate # 0 pg 1 # 1 Bulletin of the Seismological Society of America, Vol. 97, No. 3, pp. 1–, June 2007, doi: 10.1785/0120060147 E Tsunami Hazard Evaluation of the Eastern Mediterranean: Historical Analysis and Selected Modeling by Amos Salamon, Thomas Rockwell, Steven N. Ward, Emanuela Guidoboni, and Alberto Comastri Abstract Seismic sea waves in the eastern Mediterranean have been reported since written history first emerged several thousand years ago. We collected and investigated these ancient and modern reports to understand and model the typical tsunamigenic sources, with the ultimate purpose of characterizing tsunami hazard along the Levant coasts. Surprisingly, only 35% of the tsunami reports could be traced back to primary sources, with the balance remaining questionable. The tsu- namis varied in size, from barely noticeable to greatly damaging, and their effects ranged from local to regional. Overall, we list 21 reliably reported tsunamis that occurred since the mid second century B.C. along the Levant coast, along with 57 significant historical earthquakes that originated from the “local” continental Dead Sea Transform (DST) system. An in-depth evaluation shows that 10 tsunamis are clearly associated with on-land DST earthquakes, and therefore, as formerly sug- gested, they probably originated from offshore, seismogenically induced slumps. Eight tsunamis arrived from the “remote” Hellenic and Cypriot Arcs, one from Italy, and two are left with as yet unrecognized sources. A major conclusion from this work is that onshore earthquakes commonly produce tsunamis along the Levant coastline, and that analogous situations are present elsewhere in the Mediterranean, as well as along the California coast and in another regions with active faults near the coast.
    [Show full text]
  • Effects of the December 2004 Indian Ocean Tsunami on the Indian Mainland
    Effects of the December 2004 Indian Ocean Tsunami on the Indian Mainland Alpa Sheth,a… Snigdha Sanyal,b… Arvind Jaiswal,c… and Prathibha Gandhid… The 26 December 2004 tsunami significantly affected the coastal regions of southern peninsular India. About 8,835 human lives were lost in the tsunami in mainland India, with 86 persons reported missing. Two reconnaissance teams traveled by road to survey the damage across mainland India. Geographic and topological features affecting tsunami behavior on the mainland were observed. The housing stock along the coast, as well as bridges and roads, suffered extensive damage. Structures were damaged by direct pressure from tsunami waves, and scouring damage was induced by the receding waves. Many of the affected structures consisted of nonengineered, poorly constructed houses belonging to the fishing community. ͓DOI: 10.1193/1.2208562͔ MAINLAND AREAS SURVEYED The Great Sumatra earthquake of 26 December 2004 did not cause shaking-induced damage to the mainland of India, but the consequent Indian Ocean tsunami had a sig- nificant effect on the southern peninsular region of India ͑Jain et al. 2005͒. The tsunami severely affected the coastal regions of the eastern state of Tamil Nadu, the union terri- tory of Pondicherry, and the western state of Kerala. Two reconnaissance teams under- took road trips to survey the damage across mainland India. One team traveled from the Ernakulam district in Kerala, then continued south along the west coast to the southern- most tip of mainland India ͑Kanyakumari͒ and up along the east coast to Tuticorin. The coastal journey was then resumed from Nagapattinam, moved northward, and concluded at Chennai.
    [Show full text]
  • Far-Field Tsunami Hazard from Mega-Thrust Earthquakes in The
    Geophys. J. Int. (2008) 172, 995–1015 doi: 10.1111/j.1365-246X.2007.03674.x Far-field tsunami hazard from mega-thrust earthquakes in the Indian Ocean Emile A. Okal1 and Costas E. Synolakis2,3 1Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL 60208, USA. E-mail: [email protected] 2Department of Civil Engineering, University of Southern California, Los Angeles, CA 90089, USA 3Technical University of Crete, GR-73100 Chanea, Greece Accepted 2007 October 31. Received 2007 October 6; in original form 2007 March 26 SUMMARY We evaluate far-field tsunami hazard in the Indian Ocean Basin based on hydrodynamic simula- tions of ten case studies of possible mega earthquakes at the major seismic zones surrounding the basin. They represent worst-case scenarios of seismic rupture along the full extent of seismogenic faults having supported large earthquakes in the historical record. In a series of numerical experiments in which the source parameters of the 2004 Sumatra tsunami are allowed to vary one by one, while keeping the seismic moment and the fault orientation unchanged, we document that the main patterns of far-field tsunami amplitudes are remarkably robust with respect to nominal variations in such parameters as hypocentral depth, exact centroid location, and slip distribution on the fault plane. These results validate the concept of modelling case scenarios of potential future earthquakes whose source is by definition imprecise. We consider seismic sources located at the extremities of the 2004 Sumatra–Andaman rupture, namely along the southern coast of Sumatra and in the Andaman–Myanmar province; along the Makran coast of Pakistan and Iran; and also along the southern coast of Java, where the possibility of a large interplate thrust earthquake cannot be entirely dismissed.
    [Show full text]
  • Written Records of Historical Tsunamis in the Northeastern South China Sea – Challenges Associated with Developing a New Integrated Database
    Nat. Hazards Earth Syst. Sci., 10, 1793–1806, 2010 www.nat-hazards-earth-syst-sci.net/10/1793/2010/ Natural Hazards doi:10.5194/nhess-10-1793-2010 and Earth © Author(s) 2010. CC Attribution 3.0 License. System Sciences Written records of historical tsunamis in the northeastern South China Sea – challenges associated with developing a new integrated database A. Y. A. Lau1, A. D. Switzer2, D. Dominey-Howes3, J. C. Aitchison1, and Y. Zong1 1Department of Earth Sciences, The University of Hong Kong, Hong Kong SAR, China 2Earth Observatory of Singapore, Nanyang Technological University, Singapore 3Australian Tsunami Research Centre and Natural Hazards Research Laboratory, University of New South Wales, Sydney, NSW 2052, Australia Received: 15 December 2009 – Revised: 9 June 2010 – Accepted: 10 June 2010 – Published: 1 September 2010 Abstract. Comprehensive analysis of 15 previously using coastal stratigraphy and inundation modeling to help published regional databases incorporating more than validate some of the historical accounts of tsunamis as well 100 sources leads to a newly revised historical tsunami as adequately evaluate the recurrence intervals of tsunamis database for the northeastern (NE) region of the South China along the now heavily developed coastlines of the region. Sea (SCS) including Taiwan. The validity of each reported historical tsunami event listed in our database is assessed by comparing and contrasting the information and descrip- 1 Introduction tions provided in the other databases. All earlier databases suffer from errors associated with inaccuracies in translation The South China Sea (SCS) is located along the southeast- between different languages, calendars and location names. ern edge of the Eurasian Plate between 99–122◦ E and 0– The new database contains 205 records of “events” reported 25◦ N.
    [Show full text]