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Pharaonic necrostratigraphy: a review of geological and archaeological studies in the Theban Necropolis, Luxor, West Bank, Egypt
Authors:Marie-Pierre Aubry  William A Berggren  Christian Dupuis  Holeil Ghaly  David Ward  Chris King  Robert W O'B Knox  Khaled Ouda  Moustafa Youssef  Wael Fathi Galal
Institution:Department of Geology, Rutgers University, Busch Campus, Wright Laboratory, 610 Taylor Road, Piscataway, NJ 08853, USA;;Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;;Fundamental and Applied Geology, Mons Polytechnics, Wallonie-Brussels Academy, rue de Houdain, 9, 7000 Mons, Belgium;;Department of History, Department of Archeology, Faculty of Arts, Zagazig University, Zagazig, Egypt;;Crofton Court, 81 Crofton Lane, Orpington, Kent BR5 1HB, UK;;16A Park Road, Bridport, Dorset DT6 5DA, UK;;British Geological Survey, Keyworth Nottingham NG12 5GG, UK;;Department of Geology, Assiut University, Assiut, 71516 Egypt (ARE)
Abstract:We present a review of archaeological and geological studies on the West Bank as a basis for discussing the geological setting of the tombs and geologically related problems with a view to providing archaeologists with a framework in which to conduct their investigations on the restoration, preservation and management of the antique monuments. Whereas the geology of the Upper Nile Valley appears to be deceptively simple, the lithological succession is vertically variable, and we have recognized and defined several new lithological units within the upper Esna Shale Formation. We have been able to delineate lithological (shale/limestone) contacts in several tombs and observed that the main chambers in some were excavated below the Esna Shale in the Tarawan Chalk Formation. We have been able to document changing dip in the strata (warping) in several tombs, and to delineate two major orientations of fractures in the field. Investigations behind the Temple of Hatshepsut, in the Valley of the Kings and around Deir El Medina have revealed four broad regional structures. We confirm that the hills located near the Nile Valley, such as Sheik Abdel Qurna, do not belong to the tabular structure of the Theban Mountain, but are discrete displaced blocks including the Thebes Limestone, as supported by Google Earth photographs.
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