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When the Greek island of Santorini, or Thera, erupted dramatically in the seventeenth or sixteenth century BC, it produced one of the largest explosions ever witnessed by humankind. The event covered Bronze Age settlements on the island with volcanic ash, and altered the course of civilisation in the region, possibly giving rise to the legend of Atlantis. Fire in the Sea blends the thrill of scientific discovery with a popular presentation of the geology, archaeology, history, peoples and environmental setting of Santorini. It is a case study of a natural disaster that will fire the imagination. Excellent colour photographs and illustrations along with easily understandable scientific and historic details make this book highly appealing to a wide audience. It will also be useful as a supplementary text for introductory courses in earth and atmospheric science, geology, volcanology, palaeoclimatology, as well as ancient history and archaeology.
The Volcano Adventure Guide is the first book of its type. It contains vital information for anyone wishing to visit, explore, and photograph active volcanoes safely and enjoyably. Following an introduction that discusses eruption styles of different types of volcanoes, how to prepare for a volcano trip, and how to avoid volcanic dangers, the book presents guides to visiting 42 different volcanoes around the world. This section is packed full of practical information including tour itineraries, maps, transportation details, and warnings of possible non-volcanic dangers. Three appendices at the end of the book direct the reader to a wealth of further volcano resources. Aimed at non-specialist readers who wish to explore volcanoes without being foolhardy, it will fascinate amateur enthusiasts and professional volcanologists alike. The stunning colour photographs throughout the book will delight armchair travellers as well as inspire the adventurous to get out and explore volcanoes for themselves.
More than 3,500 years ago, people on the Greek island of Calliste had a very good life. They enjoyed lots of sunshine, had plenty of food, and lived in large homes. They even had running water and flush toilets. There was only one problem: Calliste was actually a volcano. Around 1650 BCE, the volcano erupted, blowing out the center of the island and creating a large bay. What was left of Calliste was buried under a thick layer of volcanic ash. Though the island was deserted for many years, people eventually returned. Several centuries ago, it was renamed Santorini. The island has reclaimed its beauty and allure, but the volcano below continues to reshape this little plot of land in the Mediterranean Sea.
This memoir synthesizes all the data from the Cambridge, Bristol and Clermont groups, and integrates data from other research groups on the caldera volcanoes of Santorini. It provides interpretations of the tectonic and magmatic evolution of Santorini. The volcanic field has been remapped and a picture of cyclic volcanic activity and magmatic evolution has emerged from this work.
This book is a collection of 22 selected papers from the homonymous Conference held in September 2003 Milos, Greece. The aim of the conference was to serve as a forum for the presentation and constructive discussion of the state-of-the-art and emerging issues on the South Aegean Volcanic Arc. In the first part of the book the tectonic- geodynamic setting and the present upper mantle structure of the Aegean area are discussed. It includes an interesting interpretation of data on the spatial distribution of intermediate focal depth earthquakes, fault plane solutions and deep velocity structures, to further investigate active tectonics related to the deep structure of the southern Aegean volcanic arc. The second part deals with general volcanological, petrological and tectonic characteristics of the SAAVA presenting an extensive review of volcanological, chemical, isotope and tectonic data, using a large amount of new field and laboratory data. Interesting conclusions are presented regarding the present volcanic associations, the volcanic fields location and shape in respect to the large tectonic lineaments and the plate motions, the source of the SAAVA parental magmas. Presented in the third part is an extensive review on the volcanic hazard assessment and the monitoring state of the SAAVA centers. Seismic and geodetic monitoring of the Santorini volcano and the recent (1995-1998) crisis of Nisyros volcano are presented and discussed. The last part deals with hydrothermal deposits and processes in the SAAVA, as well as products and processes in adjacent areas with a particular interest and significance that link them to the SAAVA processes.*Systematic re-evaluation on the geodynamic and tectonic setting of the Aegean active volcanic centers *Thorough review with new data and ideas on the magma source region, the magma differentiation processes in both the deep and shallow levels, and the volcanological processes related both to the magma composition and storage depth as well as to the tectonic regime of the volcano growth area*Up to date estimation of the volcanic hazard in the Aegean area, and a detailed presentation of the present state and the monitoring efforts of the South Aegean active centers
Discusses why and how volcanoes erupt and provides an historical account of major volcanic activity through time.
This open access book provides a comprehensive overview of volcanic crisis research, the goal being to establish ways of successfully applying volcanology in practice and to identify areas that need to be addressed for future progress. It shows how volcano crises are managed in practice, and helps to establish best practices. Consequently the book brings together authors from all over the globe who work with volcanoes, ranging from observatory volcanologists, disaster practitioners and government officials to NGO-based and government practitioners to address three key aspects of volcanic crises. First, the book explores the unique nature of volcanic hazards, which makes them a particularly challenging threat to forecast and manage, due in part to their varying spatial and temporal characteristics. Second, it presents lessons learned on how to best manage volcanic events based on a number of crises that have shaped our understanding of volcanic hazards and crises management. Third, it discusses the diverse and wide-ranging aspects of communication involved in crises, which merge old practices and new technologies to accommodate an increasingly challenging and globalised world. The information and insights presented here are essential to tapping established knowledge, moving towards more robust volcanic crises management, and understanding how the volcanic world is perceived from a range of standpoints and contexts around the globe.
This impressive scientific resource presents up-to-date information on ten thousand years of volcanic activity on Earth. In the decade and a half since the previous edition was published new studies have refined assessments of the ages of many volcanoes, and several thousand new eruptions have been documented. This edition updates the book’s key components: a directory of volcanoes active during the Holocene; a chronology of eruptions over the past ten thousand years; a gazetteer of volcano names, synonyms, and subsidiary features; an extensive list of references; and an introduction placing these data in context. This edition also includes new photographs, data on the most common rock types forming each volcano, information on population densities near volcanoes, and other features, making it the most comprehensive source available on Earth’s dynamic volcanism.