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The Apocalyptic Dimensions of Climate Change
Climate change and the apocalypse are frequently associated in the popular imagination of the twenty-first century. This collection of essays brings together climatologists, theologians, historians, literary scholars, and philosophers to address and critically assess this association. The contributing authors are concerned, among other things, with the relation between cultural and scientific discourses on climate change; the role of apocalyptic images and narratives in representing environmental issues; and the tension between reality and fiction in apocalyptic representations of catastrophes. By focusing on how figures in fictional texts interact with their environment and deal with the consequences of climate change, this volume foregrounds the broader social and cultural function of apocalyptic narratives of climate change. By evoking a sense of collective human destiny in the face of the ultimate catastrophe, apocalyptic narratives have both cautionary and inspirational functions. Determining the extent to which such narratives square with scientific knowledge of climate change is one of the main aims of this book.
Tectonic Aspects of the Alpine-Dinaride-Carpathian System
The Alps, Carpathians and Dinarides form a complex, highly curved and strongly coupled orogenic system. Motions of the European and Adriatic plates gave birth to a number of 'oceans' and microplates that led to several distinct stages of collision. Although the Alps serve as a classical example of collisional orogens, it becomes clearer that substantial questions on their evolution can only be answered in the Carpathians and Dinarides. Our understanding of the geodynamic evolution of the Alpine-Dinaride-Carpathian System has substantially improved and will continue to develop; this is thanks to collaboration between eastern and western Europe, but also due to the application of new methods and the launch of research initiatives. The largely field-based contributions investigate the following subjects: pre-Alpine heritage and Alpine reactivation; Mesozoic palaeogeography and Alpine subduction and collision processes; extrusion tectonics from the Eastern Alps to the Carpathians and the Pannonian Basin; orogen-parallel and orogen-perpendicular extension; record of orogeny in foreland basins; tectonometamorphic evolution; and relations between the Alps, Apennines and Corsica.
Evolution of the Pyrenees During the Variscan and Alpine Cycles, Volume 1
Evolution of the Pyrenees during the Variscan and Alpine Cycles 1 presents the evolution of geological knowledge of the Pyrenees as a result of major scientific research programs in the early 21st century. This book, dedicated to the Variscan cycle and Cretaceous rifting, traces the evolution of the Pyrenean domain between 340 Ma and 90 Ma. It begins with an analysis of the state of knowledge of the Pyrenean basement, whose structure is inherited from the Variscan evolution of this domain. It then traces the kinematic evolution of the western Mediterranean domain since the Paleozoic. Finally, it discusses the evolution of our knowledge of Cretaceous rifting and the sedimentary and metasomatic processes associated with the individualization of the Iberian–Eurasian plate boundary.
The Epigraphy and History of Boeotia
Over the past 20 years, Boeotia has been the focus of intensive archaeological investigation that has resulted in some extraordinary epigraphical finds. The most spectacular discoveries are presented for the first time in this volume: dozens of inscribed sherds from the Theban shrine of Heracles; Archaic temple accounts; numerous Classical, Hellenistic and Roman epitaphs; a Plataean casualty list; a dedication by the legendary king Croesus. Other essays revisit older epigraphical finds from Aulis, Chaironeia, Lebadeia, Thisbe, and Megara, radically reassessing their chronology and political and legal implications. The integration of old and new evidence allows for a thorough reconsideration of wider historical questions, such as ethnic identities, and the emergence, rise, dissolution, and resuscitation of the famous Boeotian koinon. Contributors include: Vassilios Aravantinos, Hans Beck, Margherita Bonanno, Claire Grenet, Yannis Kalliontzis, Denis Knoepfler, Angelos P. Matthaiou, Emily Mackil, Christel Müller, Nikolaos Papazarkadas, Isabelle Pernin, Robert Pitt, Adrian Robu, and Albert Schachter.
Geodynamics of the Alps 1
Geodynamics of the Alps consists of three volumes. This first volume describes the recent and present-day structure and tectonic setting of the Alpine chain, from the lithospheric mantle to brittle crust and surface topography. It also provides a historical overview of Alpine research, with two chapters covering specific Alpine regions (Corsica and the Eastern Alps) through all phases of Alpine history. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.
Geodynamics of the Alps 2
Geodynamics of the Alps consists of three volumes. This second volume presents the pre-collisional history of the Alps. It discusses the Variscan orogeny in the Alpine realm, the inferred paleo-geography, the structure and processes affecting continental margins and the mantle structure in the pre-orogenic Alpine realm. It concludes by describing oceanic and continental subduction processes. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.
Geodynamics of the Alps 3
Geodynamics of the Alps consists of three volumes. This third volume is entirely dedicated to Alpine collision. It describes and interprets elements of the Alpine chain, including Alpine magmatism, the formation of external massifs, the foreland basin, the exhumation of the internal part of the chain and the northern deformation front of the Alps. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.
Subduction Zone Geodynamics
Subduction is a major process that plays a first-order role in the dynamics of the Earth. The sinking of cold lithosphere into the mantle is thought by many authors to be the most important source of energy for plates driving forces. It also deeply modifies the thermal and chemical structure of the mantle, producing arc volcanism and is responsible for the release of most of the seismic energy on Earth. There has been considerable achievements done during the past decades regarding the complex interactions between the various processes acting in subduction zones. This volume contains a collection of contributions that were presented in June 2007 in Montpellier (France) during a conference th...
