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Contemporary natural disasters such as Hurricane Katrina are quickly followed by disagreements about whether and how communities should be rebuilt, whether political leaders represent the community’s best interests, and whether the devastation could have been prevented. Shaky Colonialism demonstrates that many of the same issues animated the aftermath of disasters more than 250 years ago. On October 28, 1746, a massive earthquake ravaged Lima, a bustling city of 50,000, capital of the Peruvian Viceroyalty, and the heart of Spain’s territories in South America. Half an hour later, a tsunami destroyed the nearby port of Callao. The earthquake-tsunami demolished churches and major buildings, damaged food and water supplies, and suspended normal social codes, throwing people of different social classes together and prompting widespread chaos. In Shaky Colonialism, Charles F. Walker examines reactions to the catastrophe, the Viceroy’s plans to rebuild the city, and the opposition he encountered from the Church, the Spanish Crown, and Lima’s multiracial population. Through his ambitious rebuilding plan, the Viceroy sought to assert the power of the colonial state over the Church, the upper classes, and other groups. Agreeing with most inhabitants of the fervently Catholic city that the earthquake-tsunami was a manifestation of God’s wrath for Lima’s decadent ways, he hoped to reign in the city’s baroque excesses and to tame the city’s notoriously independent women. To his great surprise, almost everyone objected to his plan, sparking widespread debate about political power and urbanism. Illuminating the shaky foundations of Spanish control in Lima, Walker describes the latent conflicts—about class, race, gender, religion, and the very definition of an ordered society—brought to the fore by the earthquake-tsunami of 1746.
The Fourteenth International Tsunami Symposium held from 31 July to 3 August 1989 in Novosibirsk, U.S.S.R., was sponsored by the International Union of Geodesy and Geophysics. Sixty-five scientists from 13 countries met to exchange information on recent advances in tsunami research. The Symposium was a great success due to the enthusiasm of the participants, the quality of research presented, and the great organization provided by the Soviet hosts. Teams of dedicated workers, under the fine leadership of Academician A. S. Alexseev and Dr V. K. Gusiakov, blended social and scientific activities in a memorable fashion. The 62 presentations of the Symposium were divided into six areas of research: generation (7), propagation (12), coastal effects (10), observations (11), seismics and tectonics (10), and hazard mitigation (12). A summary of the research presented appears as the first article in this special issue. Following the Symposium, a team of session chairmen nominated 20 of these oral presentations to be published in a special issue devoted to the International Tsunami Symposium.
The words and photographs of people who have witnessed tsunamis, along with the science, history, and protection efforts surrounding this watery disaster.
This Special Publication examines tsunami hazard and risk, with particular focus on using the geological record. With Earth’s growing population clustered increasingly on coastlines, tsunami hazards are of concern worldwide. The papers explore the sedimentological and dynamic traces of recent and prehistoric tsunamis globally – from Europe to the Pacific – as well as looking at historic records and how the information can be used to characterise the scale of impacts and areas that are most susceptible to tsunami hazards. Armed with this information, scientists can begin to quantify risks, both to populations and in economic terms. This volume is aimed both at scientists working in this field and at a wider community, interested in tsunami science and natural hazard assessment.
This monograph is a compilation of a number of research studies presented in fourteen chapters dealing with the impact and restoration of coastal environments that have been affected by earthquakes and tsunamis. The focus is mainly on rivers, estuaries, coastal lagoons, beaches, and related ecosystems. In addition to direct impact and response due to flooding and subsequent abrasion, this publication covers physical, chemical and biological responses in coastal morphology, water quality and ecosystems and includes also topics dealing with risk reduction and vulnerability. This compilation mainly covers examples from large magnitude earthquake and tsunami events in the Indian and Pacific Ocean that are complemented with other events in Latin America and the Iberian Peninsula. Comprehensive descriptions of multi-scale impacts of tsunami and earthquake events, both spatially and temporally, will help the reader to understand the complicated interactions which occur in coastal zones in order to create a sustainable, resilient environment and achieve a society with smart post-event recovery planning. This book is aimed at researchers and students in coastal science and engineering as well as at policy makers, environmental planners and coastal managers.
It is a comprehensive and well illustrated textbook on all aspects of tsunami. I don't think there is any other book on the topic published. As one bookseller said after the Indian Ocean tsunami event, "I would have just filled my front window with copies and they would have walked out the store." This statement was just as relevant after the Japanese tsunami of 2011 and will be as relevant when the next large tsunami event happens, sooner rather than later. The book can be used by a student or layperson to gain encyclopedic knowledge about tsunami.
The 2004 Indian Ocean tsunami was triggered by a 9. 15 magnitude earthquake (MELTZNER et al. , 2006; CHLIEH et al. , 2007) that occurred at 0:58:53 GMT, 7:58:53 LT (USGS) (t ). The epicenter was located at 3. 3 N, 95. 8 E (Fig. 1) with a focal depth of EQ approximately 30 km. The earthquake was responsible for a sudden fault slip estimated on average from 12–15 m (SYNOLAKIS et al. , 2005; LAY et al. , 2005) to 20 m (FU and SUN, 30 2006). The seismic moment estimate (Mo = 1. 3 5 9 10 dyne-cm), based on the Figure 1 Locations of video recordings, recovered clocks, and reliable eyewitness observations. 1: Coastal plains ?ooded by the tsunami; 2: non-?ooded coastal plains; 3: uplands. Insert 3D-map showing the Sumatra Island, the studied area, and the epicenter of the 26/12/2004 earthquake. The video taken at Uteuen Badeue, on the eastern edge of the Banda Aceh Bay, was recorded by the chief of the Fishery Regional Of?ce from the top of a cliff. The movie that was shot near the Baiturrahman mosque in downtown Banda Aceh has been shown worldwide on TV. The one at Peukan Bada has been recorded during a wedding party. The last two movies were analyzed in detail in order to calculate the tsunami velocity (FRITZ et al. , 2006). Vol.