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Discovery of the causeway and the mortuary temple of the Pyramid of Amenemhat II using near‐surface magnetic investigation,Dahshour, Giza,Egypt
Authors:T. Abdallatif  A.E. El Emam  M. Suh  I.A. El Hemaly  H.H. Ghazala  E.H. Ibrahim  H.H. Odah  H.A. Deebes
Affiliation:1. Department of Geomagnetism and Geoelectricity, National Research Institute of Astronomy and Geophysics (NRIAG), El‐Marsd Street, Helwan, 11722‐138 Cairo, Egypt;2. Department of Geoenvironmental Sciences, Kongju National University, 309, Research Building, 182 Sinkwan‐dong, Kongju, Chungnam 314‐701, South Korea;3. Department of Geology, Faculty of Science, Mansoura University, 35516 Mansoura, Egypt;4. College of Tourism and Archaeology, King Saud University, P.O. Box 2627, Riyadh 7524‐12372, Saudi Arabia
Abstract:The main outbuildings of the Amenemhat II pyramid complex in Dahsour were yet to be discovered due to a very long subjection of the area to the military authorities and also the demolition of the pyramid itself. We describe the discovery of some of these outbuildings using near‐surface magnetic investigations. A gradiometer survey was conducted in the area east of the pyramid to measure the vertical magnetic gradient with a high resolution instrument at 0.5 m sampling interval. The data showed some undesirable field effects such as grid discontinuities, grid slope, traverse stripe effects, spikes and high frequencies originating from recent ferrous contamination. These undesirable effects were addressed to produce an enhanced display. We have successfully detected four main structures in the area east of the pyramid; the causeway that connected the mortuary temple with the valley temple during the Middle Kingdom of the 12th Dynasty, the mortuary temple and its associated rooms, ruins of an ancient working area and an Egyptian‐style tomb structure called a Mastaba. An improved recognition for these structures was accomplished by using the analytic signal and Euler deconvolution techniques. Excavation of a small part within the study area has proven the reliability of magnetic discoveries and the shallowness and composition of the detected features.
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