Abstract

An archeological study using magnetic and ground-penetrating radar methods has been performed at the Dahshour region (Giza, Egypt), where various covered structures have not been found because of the long coercion of the zone under the military specialists. Dahshour is the southern extension of the Saqqara and Giza Pyramids plateau, around 25 km south of Cairo. The area is known for its colored pyramids—the white, red, and black pyramids, and the famous Bent Pyramid. Four investigation sites were chosen around the Bent Pyramid complex. The geophysical investigation has revealed the presence of some buried structures made up of mud bricks such as tombs, mud-brick walls, causeway, and remains of an ancient temple. Numerous limestone blocks were also detected. The study indicates the possible existence of an older valley temple made up of mud bricks and confirms the existence of another causeway that led to the Nile Valley. To protect the Egyptian heritage around this vital area, a detailed computation of the current crustal stress/strain state has been performed by taking into account all the available GPS observations. Achieved results indicated that the southern and the southeastern sectors of the investigated area are currently accumulating strain, and this means that there is a possibility for future earthquakes to occur around this vital archaeological area. Buried structures are preserved by confinement in the burial materials like a large mold. However, external load or stress can still cause damage. Therefore, during excavation, the stress should be reduced to avoid wall collapsing and structure damage. Therefore, it is recommended to start excavation from the stress direction from the southern side.

Highlights

  • Dahshour area is located southwest of Cairo (Figure 1A) within the Giza governorate, which is acclaimed for one of the seven world marvels, the pyramids of Giza

  • The study area belongs to the Bent Pyramid complex structure area

  • Seismic hazard assessment studies are performed for structures rising above the ground surface where they are usually affected by ground shaking

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Summary

INTRODUCTION

Dahshour area is located southwest of Cairo (Figure 1A) within the Giza governorate, which is acclaimed for one of the seven world marvels, the pyramids of Giza. Abdallatif et al (2010) have conducted nearsurface magnetic investigations using the FM36 magnetic gradiometer in the area east of the Amenemhat II pyramid They scan an area of 340 m × 200 m, which comprises four major archaeological features of different shapes and sizes that mostly consist of mud bricks. The ground-penetrating radar (GPR, SIR-2000), the electrical resistance meter (Geoscan RM15), and the electromagnetic profiler (GEM300) have been utilized to acquire some geophysical data within the area scanned by Abdallatif et al (2010) These techniques have been applied to selected zones to investigate specific objects and oriented to solve the problems questioned by the local archaeological inspectors. Within Site B, a chosen area of 20 m × 40 m (see Supplementary Figure S5a) was further scanned using GPR to outline and follow the anomalies that appear in the magnetic survey. The data were processed annually; that is, the parameters of the crustal deformation were computed for every year and for the total period from 2005 to 2011 to compute the mean velocity at each station

Magnetic Survey Results
GPR Survey Results
GPS Results
CONCLUSIONS AND DISCUSSIONS
DATA AVAILABILITY STATEMENT
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