2010
DOI: 10.2113/gssgfbull.181.3.279
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Geological and topographical study of the original hills at the base of Fourth Dynasty Egyptian monuments of the Memphite plateau

Abstract: Rock foundations of the Kephren and Kheops pyramids are examined in comparison with other Fourth Dynasty monuments: the Sphinx, Queen Kentkawes' monument and the Abu Rawash monument. This study is based on geological and topographical observations, photomontages and field measurements. The results, which are correlated with those of former studies, demonstrate the existence of natural hills used as substrata in the construction of the two great pyramids. The minimum volume of these hills can be estimated at 12… Show more

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Cited by 6 publications
(5 citation statements)
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“…Here we show how the base of the Pyramid was reinforced by the incorporation of the outcrop, and that the concavity strengthens the struc-ture of the whole pyramid including the base. The Great Pyramid was built on a natural carved outcrop whose volume is estimated to be about 20 percent of the monument (Raynaud et al, 2008). Let us present our idea that how they incorporated this outcrop into the monument for its stability.…”
Section: Tightening the Pyramid By Reinforced Base And Concavitymentioning
confidence: 99%
“…Here we show how the base of the Pyramid was reinforced by the incorporation of the outcrop, and that the concavity strengthens the struc-ture of the whole pyramid including the base. The Great Pyramid was built on a natural carved outcrop whose volume is estimated to be about 20 percent of the monument (Raynaud et al, 2008). Let us present our idea that how they incorporated this outcrop into the monument for its stability.…”
Section: Tightening the Pyramid By Reinforced Base And Concavitymentioning
confidence: 99%
“…It is situated on a calcareous plateau and occupies an area of 90 km 2 , 8 km northwest of the Giza Pyramids. The area consists in sedimentary rocks, basalt flows, and loose sediments (multiple kinds of limestone, sandstone, basalt, and clay) [36,37]. Abu-Rawash is a famous site due to the presence of the pyramid of King Djedefre, the third king of the 4th Dynasty during the Old Kingdom (2566-2558 BC), which is the son and successor of the Pharaoh Cheops (Khufu) [38,39].…”
Section: The Archaeological Areamentioning
confidence: 99%
“…3); in this case, the role of the geoheritage worker is to translate scientific observation to the popular interpretation of such "geomorphs." An example where geologic impact is deemed essential to understanding archaeological sites would include the Sphinx, now speculated to be built upon a geologic formation that inspired its construction (Raynaud et al, 2008), as well as the presence of the geomorphs of bulls' horns that possibly influenced the location of the Knossos site of Crete (Schama, 1995).…”
Section: Components Of Geoheritagementioning
confidence: 99%