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The Dead Sea
Located 400 meters below sea level, at the tectonically active irregular boundary between the Mediterranean and Arabic plates, the Dead Sea is the site of many interesting phenomena. It provides a modern analog for ancient pull-apart basins and allows researchers to examine the process of evaporite deposition from deep water. It also offers insight into the adaptive ability of the life form living in the hypersaline brine. This book, based on a conference held in Tel Aviv in December 1993, focuses on the geophysics, geochemistry, hydrology, and climatology of the Dead Sea region.
Tectonic Development of the Eastern Mediterranean Region
The Eastern Mediterranean region is a classic area for the study of tectonic processes and settings related to the development of the Tethyan orogenic belt. The present set of research and synthesis papers by earth scientists from countries in this region and others provides an up-to-date, interdisciplinary overview of the tectonic development of the Eastern Mediterranean region from Precambrian to Recent. Key topics include continental rifting, ophiolite genesis and emplacement, continental collision, extensional tectonics, crustal exhumation and intra-plate deformation (e.g. active faulting). Alternative tectonic reconstructions of the Tethyan orogen are presented and discussed, with important implications for other regions of the world. The book will be an essential source of information and interpretation for academic researchers (geologists and geophysicists), advanced undergraduates and also for industry professionals, including those concerned with hydrocarbons, minerals and geological hazards (e.g. earthquakes).
Foundation, Fall and Flood
Science and the Bible do not contradict one another. The author shows that the plain and literal text of the Bible is in perfect harmony with even the latest findings of mainstream science. You need not compromise either your faith or your intellect.
A Companion to the Environmental History of Byzantium
How did humans and the environment impact each other in the medieval Eastern Mediterranean? How did global climatic fluctuations affect the Byzantine Empire over the course of a millennium? And how did the transmission of pathogens across long distances affect humans and animals during this period? This book tackles these and other questions about the intersection of human and natural history in a systematic way. Bringing together analyses of historical, archaeological, and natural scientific evidence, specialists from across these fields have contributed to this volume to outline the new discipline of Byzantine environmental history. Contributors are: Johan Bakker, Henriette Baron, Chryssa Bourbou, James Crow, Michael J. Decker, Warren J. Eastwood, Dominik Fleitmann, John Haldon, Adam Izdebski, Eva Kaptijn, Jürg Luterbacher, Henry Maguire, Mischa Meier, Lee Mordechai, Jeroen Poblome, Johannes Preiser-Kapeller, Abigail Sargent, Peter Talloen, Costas Tsiamis, Ralf Vandam, Myrto Veikou, Sam White, and Elena Xoplaki
The Afar Volcanic Province Within the East African Rift System
The seismically and volcanically active East African Rift System is an ideal laboratory for continental break-up processes: it encompasses all stages of rift development. Its northernmost sectors within the Afar volcanic province include failed rifts, nascent sea-floor spreading, and youthful passive continental margins associated with one or more mantle plumes. A number of models have been proposed to explain the success and failure of continental rift zones, but there remains no consensus on how strain localizes to achieve rupture of initially 125-250 km-thick plates, or on the interaction between the plates and asthenospheric processes. This collection of papers provides new structural, stratigraphic, geochemical and geophysical data and numerical models needed to resolve fundamental questions concerning continental break-up and mantle plume processes. The focus is on how mantle melt intrudes and is distributed through the plate, and how this magma intrusion process controls along-axis segmentation and facilitates break-up.
Carbonate-Clastic Transitions
Over the years, the field of sedimentology has become subdivided into various specialities. Two of the largest groups are those who study clastic rocks and those who study carbonates. There is little communication between the two: journals appear which are exclusively devoted to one or the other, and research conferences tend to be mutually exclusive. On the other hand, rocks themselves cannot be "pigeon-holed" in this way - the facies change from clastic to carbonate both laterally and through time. This volume stems from the editors' observations of such changes in the Gulf of Mexico and their realization that these geologically important transitions were being largely ignored because of p...
The TRANSMED Atlas. The Mediterranean Region from Crust to Mantle
A publication of the Mediterranean Consortium for the 32nd International Geological Congress
Evolution of the Levant Margin and Western Arabia Platform Since the Mesozoic
This volume combines original data from the offshore and onshore Levant in various fields like sedimentology, palaeontology, geochemistry, structural geology and geophysics. This multidisciplinary approach provides an overview of the development of the Levant Basin and allows discussion of the later geological history and deformation processes of the Levant provinces
