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

Over eighty contributions from leading researchers review 2.5 million years of environmental change and human cultural evolution in the Levant.

In this comprehensive final report David Ilan and 12 other contributing authors present the rich finds from the Iron Age I (circa 1200-950 BCE) levels at Tel Dan, gleaned in the course of Avraham Biran's 1966-1999 excavations at the site. The architecture, ceramics, metal, flint, bone and ground stone objects and ecofacts, all contribute to the portrayal of a cosmopolitan society that thrived, initially, under Egyptian imperial rule, subsequently forging its own way with the departure of Egyptian hegemony. The early Iron Age levels at Tel Dan show material evidence for the presence of local peoples, Egyptians, Cypriots, Aegeans, and Syrians, who together, negotiated a new identity, as Danites.

This volume presents results of a variety of case studies documenting the Late Palaeozoic climate changes and cyclicity of deposition. The collected papers cover many aspects related to palaeoenvironmental analysis with sedimentological, stratigraphic, palaeobiological, geochemical, and palaeomagnetic studies of the fossil record around the Late Palaeozoic Ice Age and soon after. They span a stratigraphic interval from Carboniferous to Permian–Triassic transition around the world. This book comprising results for a range of disciplines, is a valuable source for not only researchers who are actively working on specific aspects of the Late Palaeozoic and looking for an up-to-date reference on this inhospitable time in the Earth’s history. It is also of interest to climate modellers and the wider scientific community with an interest in the latest research on the decline of the Palaeozoic World.

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.