Egypt During The Last Interglacial

by Fred Wendorf, Romuald Schild and Angela E. Close INTRODUCTION roughly contemporaneous with the later part of Isotope Stage 7; most sites occur in sediments dated between 100 The Middle Paleolithic is potentially one of the most and 130 ka and fall early in the Last Interglacial; the most interesting periods in human history. It marks a major recent Middle Paleolithic site dates between 70 and 80 ka. at break from the long period of the Lower Paleolithic when the end of the Last Interglacial. there was essentially no change for several hundreds of thousands of years, and it was during the Middle THE MODERN ENVIRONMENT Paleolithic, and probably early in that stage, that the The two depressions of Bir Tarfawi and Bir Sahara East are modem form of human being first appeared in Africa (Stringer and Andrews 1988). We do not know whether the near the center of the southern Libyan Desert. They are earliest modem Africans behaved differently from Middle about 350 km southwest of Kharga Oasis, and the same Paleolithic people elsewhere in the world and of different distance west and slightly north of Abu Simbel, at 22°55'N, physical types, but we should find out. A study of human 28°45'E.

An analytical bibliography that contains 7407 references, covering the Egyptian prehistory (palaeolithic, neolithic and predynastic) as well as the period of the first two dynasties.

The Encyclopedia of Prehistory represents also defined by a somewhat different set of an attempt to provide basic information sociocultural characteristics than are eth on all archaeologically known cultures, nological cultures. Major traditions are covering the entire globe and the entire defined based on common subsistence prehistory of humankind. It is designed as practices, sociopolitical organization, and a tool to assist in doing comparative material industries, but language, ideology, research on the peoples of the past. Most and kinship ties play little or no part in of the entries are written by the world's their definition because they are virtually foremost experts on the particular areas unrecoverable from archaeological con and time periods. texts. In contrast, language, ideology, and The Encyclopedia is organized accord kinship ties are central to defining ethno ing to major traditions. A major tradition logical cultures. is defined as a group of populations sharing There are three types of entries in the similar subsistence practices, technology, Encyclopedia: the major tradition entry, and forms of sociopolitical organization, the regional sub tradition entry, and the which are spatially contiguous over a rela site entry. Each contains different types of tively large area and which endure tempo information, and each is intended to be rally for a relatively long period. Minimal used in a different way.

Over the last decade, Africa has taken a central position in the search for the timing and mechanisms leading to modern human origins, and the rich archaeological and human paleontological record of North Africa is critical to this search. In this volume, we bring together new research into the archaeology, human paleontology, chronology, and environmental context of modern human origins in North Africa. The result is a volume that better integrates the North African record into the modern human origins debate and at the same time highlights the research questions that are currently the focus of continued work in the area.​

Processual archaeologists seek to explain variability in the static archaeological record we observe in the present as a necessary first step toward learning how to learn about the operation of cultural dynamics in the past. The approach is a diverse and productive one that focuses on developing learning strategies. Researchers pursuing processual archaeology have already discovered a great deal about the archaeological record and about past dynamics, and there is a huge potential for building on the foundation laid thus far. The contributors to this volume provide clearly written research articles that are easily accessible to upper-level undergraduates and professional archaeologists. Although the papers do not focus on a single region, time period, or domain of observation (e.g. settlement patterns or lithics or site structure), they are integrated by shared goals for archaeology. This book clearly demonstrates that processual archaeology, far from having been replaced by post-processual archaeology, is becoming more and more powerful as our analytic sophistication and knowledge of the archaeological record grow.

The Phanerozoic Geology and Natural Resources of Egypt includes a series of chapters written by highly qualified group of researchers whose expertise is recognized and appreciated not only in Egypt, but also in the world over. The chapters span a wide range of geological subdisciplines including tectonics, paleogeography, stratigraphy, sedimentology, paleontology, groundwater, and energy resources, just to name a few. In this regard, the book provides the reader with ample knowledge about the different facets of the fascinating and always intriguing geology of Egypt since the Precambrian time. For a junior researcher or a geoscience student, the book is a comprehensive, multidisciplinary one-stop resource that they will continue to reference and rely on for years to come. For a more experienced scientist, the book summarizes the current state of knowledge, highlights the magnitude of complexity of the geology of Egypt and northeast Africa, and reveals potential areas where future research should be directed. The book is written in simple, easy to understand English language and contains very useful high-quality illustrations. Last but not least, The Phanerozoic Geology and Natural Resources of Egypt has been reviewed and edited by world class, highly ranked geoscientists from Egypt, Europe, and USA.

by Fred Wendorf and Romuald Schild The Eastern Sahara is a fascinating place to study structures. These larger, more complex sites are almost prehistory. Confronted with the stark reality of a hyper always in the lower parts of large basins, most of which arid environment that receives no measurable rainfall, were formed by deflation during the Late Pleistocene lacks vegetation, and is seemingly without life, it would hyper-arid interval between about 65,000 and 13,000 seem to be an unlikely place to find a rich and complex years ago. Their location near the floor of these basins mosaic of archaeological remains documenting past was influenced primarily by one factor - water. During human presence. Despite this impression of a hostile wet phases, runoff from extensive catchment areas environment, there is widespread and abundant caused the development of large, deep, seasonal lakes, archaeological evidence. or playas, in the lowermost parts of these basins. This It is obvious that this area was not always a lifeless surface water would last for several weeks or months desert. Faunal and plant remains found in the excavations after the seasonal rains, and by digging wells after the at Holocene-age settlements, dating between 9500 and playa became dry, water could still be obtained during 5000 radiocarbon years ago, indicate that rainfall during most, if not all, of the dry season.