Through an analysis of recently discovered Ptolemaic pottery from Mut al-Kharab, as well as a reexamination of pottery collected by the Dakhleh Oasis Project during the survey of the oasis from 1978–1987, this book challenges the common perception that Dakhleh Oasis experienced a sudden increase in agricultural exploitation and a dramatic rise in population during the Roman Period. It argues that such changes had already begun to take place during the Ptolemaic Period, likely as the result of a deliberate strategy directed toward this region by the Ptolemies. This book focuses on the ceramic remains in order to determine the extent of Ptolemaic settlement in the oases and to offer new insights into the nature of this settlement. It presents a corpus of Ptolemaic pottery and a catalogue of Ptolemaic sites from Dakhleh Oasis. It also presents a survey of Ptolemaic evidence from the oases of Kharga, Farafra, Bahariya and Siwa. It thus represents the first major synthesis of Ptolemaic Period activity in the Egyptian Western Desert.

Scholars from Egypt, Germany and the US review and analyze the results of work carried out on the geology of Egypt: geomorphology and evolution of landscape, tectonics, geophysical regime, volcanicity, Precambrian geology, geologic history and paleogeography, paleontology of selected taxa, ore depos

This is the only volume to present significant results of research into the Pleistocene of the Western Desert of Egypt. Research on Pleistocene prehistoric remains in Dakhleh Oasis began during survey in the 1978 Dakhleh Oasis Project (DOP) season, with discovery of the ubiquity of stone artefacts. Dedicated work by both prehistorians and environmentalists continued until 2011. Comparative DOP reconnaissance and geological work in Kharga Oasis began in 1987, which morphed into the Kharga Oasis Prehistory Project (KOPP) in 2001. Papers on the Pleistocene research are focused on geoarchaeological and palaeo-environmental data, reporting on different aspects of the off-site fieldwork conducted in the oases. Pleistocene finds and sequence are included. Detailed analyses of palaeolakes, the meteoritic Dakhleh Event, chronometric dating, and the 'empty desert hypothesis' employ state of the art research strategies and techniques to provide important information on Pleistocene human uses and habitability in the Western Desert. A summary paper and a Catalogue of Pleistocene localities recorded in the Dakhleh Oasis survey are provided. The volume will be a major contribution to the publication of the results of several decades of work in a region where fieldwork is now increasingly difficult. This will be the only volume in which the significant results of the research into the Pleistocene of the Western Desert of Egypt appear. This has been undertaken under the auspices of the Dakhleh Oasis Project and its off-shoot The Kharga Oasis Prehistory Project. The preliminary results have been presented at various conferences and in articles that have all been well received. They incorporate state of the art research strategies and dating techniques. The volume will be a major contribution to the publication of the results of several decades of work in a region where fieldwork is now increasingly difficult.

This richly illustrated book provides an overview of the Neoproterozoic Pan-African Belt of Egypt (PABE), which represents the northwestern continuation of the Arabian-Nubian Shield (ANS) and the East African Orogen (EAO). The first chapter offers an introduction to the Turin Papyrus Map and the historical background of the PABE, while the second addresses how the PABE is related to the ANS and EAO. Rock succession of the PABE is dealt with in Chapter 3, while Chapter 4 focuses on Sinai Metamorphic Core Complexes and implications on the break-up of Rodinia. Subsequent chapters discuss a broad range of topics, e.g. ophiolite-dominated suprastructural rocks; volcanosedimentary succession, Neoproterozoic volcanism and volcanic rocks in Egypt; enigmatic issues concerning granite, Dokhan and Hammamat sediments; the lithospheric mantle beneath the Northeast African continent and the mantle section of Neoproterozoic ophiolites from the PABE; sutures, megashears and petrogenetic evolution of the Neoproterozoic rocks of Egypt; and metallic and non-metallic mineral deposits in the PABE, which are covered in extensive detail. The book’s closing chapters discuss the application of remote sensing techniques and anisotropy of magnetic susceptibility (AMS) to decipher the tectonic evolution of the PABE, as well as the use of geophysical data to map structural features and hydrothermal alteration zones in the PABE.