"Ancient earthquakes are pre-instrumental earthquakes that can only be identified through indirect evidence in the archaeological (archaeoseismology) and geological (palaeoseismology) record. Special Paper 471 includes a selection of cases convincingly illustrating the different ways the archaeological record is used in earthquake studies. The first series of papers focuses on the relationship between human prehistory and tectonically active environments, and on the wide range of societal responses to historically known earthquakes. The bulk of papers concerns archaeoseismology, showing the diversity of approaches, the wide range of disciplines involved, and its potential to contribute to a better understanding of earthquake history. Ancient Earthquakes will be of interest to the broad community of earth scientists, seismologists, historians, and archaeologists active in and around archaeological sites in the many regions around the world threatened by seismic hazards. This Special Paper frames in the International Geoscience Programme IGCP 567 'Earthquake Archaeology: Archaeoseismology along the Alpine-Himalayan Seismic Zone.'"--Publisher's description.

The New Madrid earthquakes of 1811–12 were the strongest temblors in the North American interior in at least the past five centuries. From the Great Plains to the Atlantic Coast and from the Great Lakes to the Gulf of Mexico, a broad cast of thinkers struggled to explain these seemingly unprecedented natural phenomena. They summoned a range of traditions of inquiry into the natural world and drew connections among signs of environmental, spiritual, and political disorder on the cusp of the War of 1812. Drawn from extensive archival research, Convulsed States probes their interpretations to offer insights into revivalism, nation remaking, and the relationship between religious and political authority across Native nations and the United States in the early nineteenth century. With a compelling narrative and rigorous comparative analysis, Jonathan Todd Hancock uses the earthquakes to bridge historical fields and shed new light on this pivotal era of nation remaking. Through varied peoples' efforts to come to grips with the New Madrid earthquakes, Hancock reframes early nineteenth-century North America as a site where all of its inhabitants wrestled with fundamental human questions amid prophecies, political reinventions, and war.

When the volcano Tambora erupted in Indonesia in 1815, as many as 100,000 people perished as a result of the blast and an ensuing famine caused by the destruction of rice fields on Sumbawa and neighboring islands. Gases and dust particles ejected into the atmosphere changed weather patterns around the world, resulting in the infamous ''year without a summer'' in North America, food riots in Europe, and a widespread cholera epidemic. And the gloomy weather inspired Mary Shelley to write the gothic novel Frankenstein. This book tells the story of nine such epic volcanic events, explaining the related geology for the general reader and exploring the myriad ways in which the earth's volcanism has affected human history. Zeilinga de Boer and Sanders describe in depth how volcanic activity has had long-lasting effects on societies, cultures, and the environment. After introducing the origins and mechanisms of volcanism, the authors draw on ancient as well as modern accounts--from folklore to poetry and from philosophy to literature. Beginning with the Bronze Age eruption that caused the demise of Minoan Crete, the book tells the human and geological stories of eruptions of such volcanoes as Vesuvius, Krakatau, Mount Pelée, and Tristan da Cunha. Along the way, it shows how volcanism shaped religion in Hawaii, permeated Icelandic mythology and literature, caused widespread population migrations, and spurred scientific discovery. From the prodigious eruption of Thera more than 3,600 years ago to the relative burp of Mount St. Helens in 1980, the results of volcanism attest to the enduring connections between geology and human destiny. Some images inside the book are unavailable due to digital copyright restrictions.

Earthquakes and Coseismic Surface Faulting on the Iranian Plateau is a comprehensive and well-illustrated multi-disciplinary research work that analyzes the human and physical aspects of the active faults and large-magnitude earthquakes since ancient times on the Iranian Plateau. The long-term historical, archaeological, and sociological record of earthquakes discussed here gives insight into earthquake magnitudes, recurrences, fault segmentation, clustering, and patterns of coseismic ruptures from prehistoric times to the present. The first part of the book examines oral traditions and literature of the region concerned with earthquakes, particularly in folklore, epic literature, and theology. The second part assesses dynamic phenomena associated with earthquakes, including active tectonics, archaeoseismicity, and coseismic surface faulting throughout the twentieth century. This work is a valuable technical survey and an essential reference for understanding seismic hazard analysis and earthquake risk minimization in earthquake-prone developing and developed countries throughout the world. - Provides a reference for seismic hazard evaluation and analysis - Covers data dealing with crustal deformations caused by earthquake faulting and folding since historic times - Presents unique and complete data for use in empirical relation analyses in all regions

Interdisciplinary study on the role of earthquakes in the eastern Mediterranean Does the “Minoan myth” still stand up to scientific scrutiny? Since the work of Sir Arthur Evans at Knossos (Crete, Greece), the romanticized vision of the Cretan Bronze Age as an era of peaceful prosperity only interrupted by the catastrophic effects of natural disasters has captured the popular and scientific imagination. Its impact on the development of archaeology, archaeoseismology, and earthquake geology in the eastern Mediterranean is considerable. Yet, in spite of more than a century of archaeological explorations on the island of Crete, researchers still do not have a clear understanding of the effects of earthquakes on Minoan society. This volume, gathering the contributions of Minoan archaeologists, geologists, seismologists, palaeoseismologists, geophysicists, architects, and engineers, provides an up-to-date interdisciplinary appraisal of the role of earthquakes in Minoan society and in Minoan archaeology – what we know, what are the remaining issues, and where we need to go. Contributors: Tim Cunningham (Université catholique de Louvain), Jan Driessen (Université catholique de Louvain), Charalampos Fassoulas (Natural History Museum of Crete, University of Crete), Christoph Grützner (RWTH Aachen University, University of Cambridge), Susan E. Hough (U.S. Geological Survey), Simon Jusseret (The University of Texas at Austin, Université catholique de Louvain), Colin F. Macdonald (The British School at Athens), Jack Mason (RWTH Aachen University), James P. McCalpin (GEO-HAZ Consulting Inc.), Floyd W. McCoy (University of Hawaii – Windward), Clairy Palyvou (Aristotle University of Thessaloniki), Gerassimos A. Papadopoulos (National Observatory of Athens), Klaus Reicherter (RWTH Aachen University), Manuel Sintubin (KU Leuven), Jeffrey S. Soles (University of North Carolina – Greensboro), Rhonda Suka (Research Corporation of the University of Hawaii), Eleftheria Tsakanika (National Technical University of Athens), Thomas Wiatr (RWTH Aachen University, German Federal Agency for Cartography and Geodesy).

Research on historical earthquakes and tsunamis in the Iberian Peninsula has made great strides in recent years, from diverse scientific fields ranging from geology to archaeology. In addition to the famous earthquake and tsunami of 1755, which intensely affected the peninsula, researchers are conducting a growing number of surveys and case studies on seismic episodes and extreme wave events of possible tsunamigenic origin in Portugal and Spain during the ancient, medieval, and modern eras. However, the development of these studies has suffered due to a certain lack of communication among the different fields of research, which are focused on their own methodologies and interests. The aim of this book is to promote interdisciplinary dialogue by linking the results of the most recent research into historical earthquakes and tsunamis in Iberia from the fields of geology, history and archaeology. The volume, which devotes special attention to tsunamis and to events that occurred in the Iberian Peninsula before 1755, offers synthetic insights, updates, and case studies of maximum interest for knowledge of the historical seismology of Portugal and Spain.