Discovery of fossils on the Giza Plateau
Text by Antoine Gigal and Sherif El Morsy
A convincing clue proving that the Giza plateau was once covered by the sea is being studied, along with other evidence of erosion due to saturation by deep water of the surface of the plateau. An echinoid (a type of sea urchin or shallow marine creature) petrified in “recent times” has been found embedded upright in the upper surface of a block adjoining the Menkaura pyramid and within the ancient intertidal range. This is a splendid discovery by an Egyptian researcher.
"I am very proud to present to you a first report on the splendid discovery by Mr Sherif el Morsi. For several reasons: first, because it is only the beginning of seriously questioning dating and other data which have been wrong for years, and because this is very thorough work based on proofs that become stronger every day. It is time for science to get its message across! I am very happy also that this is an Egyptian discovery because Egyptian researchers and scientists well deserve it.
A more personal reason is that for the last 20 years now I have also been collecting evidence of sea erosion due to deep water saturation on the Giza plateau. My own theory (already published in France in 2007) is that the last Great Flood (and no doubt others before it) came up the Giza plateau, and that the Ancient Egyptians with their incomparable skills adapted the plateau from the beginning in order to protect their population and their science beneath it."
Report from Mr Sherif El Morsi (+ more informations about Mr Sherif El Morsi on gizaforhumanity.org)
“I have spent the past 12 years doing on-site research in the Giza Necropolis. My research has brought some important discoveries such as the Neolithic honeycombed community of cavern dwellers on the Great Pyramid eastern escarpment, the megalith ramp used for hauling the granite blocks up the escarpment to be used in the construction of the Kings chamber, and just recently the different extensive erosion patterns found on different elevations in the Giza plateau with an existing ancient shoreline.
I Like to thank Ms. Antoine Gigal for this honourable invitation to put on her prestigious board my following work. I am following the footsteps of the renown geologist Dr. Schoch and the great writer/journalist Graham Hamcock, but expanding their theory that is based on erosion patterns found on the Sphinx body due to water erosion. I have found that the extensive erosion patterns at the lower elevations of the plateau are different to the erosion patterns found at higher elevations. These erosion patterns are due to the Necropolis’s inundation by water. The inundation of water reaches a maximum of 75 meters over our current sea level creating a shoreline at the Khafra enclosure that spans all the way across to the Menkara temple. This shoreline is a 2 meter high intertidal range showing pitting and tidal notches due to seawater, wave mechanics, and tidal ebbing. At the lower levels such as at the Sphinx, the Sphinx temple, the first 20 courses of the Great pyramid including the boat pits; we see erosion due to deeper water saturation, where the stone blocks and wall linings have absorbed sea water. As the waters receded and a dry sunny windy climate took place, these megalithic stone blocks started weathering, creating tafoni erosions which are due to the salt chemically reacting and flaking the limestone with pitting formations. During a catastrophic sea surge and the forthcoming water regression, we clearly observe at certain areas such as corners, outlets, and trenches... horizontal indentures due to water force gushing and turbulence. On the top temple blocks we have sediment and alluvium deposits that have collected on the flat surfaces such as seen in shallow sea beds and lagoons, creating an oozing spongy effect due to the water regression that left these deposits.
Reaching the maximum level of the inundation, which is 75 meters over our current sea level, we see a different type of erosion that is due to wave mechanics and tidal ebbing that has created a 2 meter high ancient intertidal range. This ancient shoreline spans from the Khafra enclosure up to the Menkara temple, where the rock hewn cliffs plus the temple blocks are all extensively eroded with tidal notches and extensive pitting. The erosions are so extensive that most blocks are nearly dilapidated out of existence, losing block mass and disfigured into grotesque shapes. This disfiguration is due to wave hitting, sea spray, and shallow marine habitation.
During my photo shoot of this ancient seashore line, I nearly tripped off a 2nd level temple block. To my surprise the bulge on the top surface of the block that nearly made me trip was a petrified exoskeleton of what seems to be an Echinoid (sea urchin), which is a shallow sea marine creature. The coincidence to discover a petrified shallow marine creature laying on a top surface of a temple block that sits right under the ancient intertidal range, is a blessing. This is probably the most absolute proof that the Giza Necropolis was inundated by a sea surge. The petrified Echinoid and the dilapidated temple block stand together creating for us such a solid picture of an ancient lagoon that once existed at the Menkara temple during a high sea that inundate the Necropolis.
Since the Mokattam limestone is formed out of miniscule fragmented marine shells such as numulites and echinoids that date back to the Eocene Epoch which is circa 30 million years ago, geologists and archeologists are debunking this discovery believing that this petrified marine creature has eroded out of the limestone block. I disagree due to these forth coming points; first, this petrified marine creature’s exoskeleton is in pristine condition with minute details of the shell perforation showing clearly, therefore it must have been exiting from a much later date such as the Pleistocene or early Holocene periods. Second, this petrified creature is laying gravitational flat in its natural sitting position on the surface of this temple block. Third, it is living in its natural environment which is in the intertidal range in a shallow lagoon with sea bed sediments. Fourth, it is not a miniscule fragment like most shells that make the limestone formation, but a large entire specimen.
In the upcoming image we can clearly see the petrified shallow marine creature sitting normally on the flat surface of the second level temple block, protruding 6 centimeters over the surface. In the back ground we have another perspective of the third level temple blocks that make these gargantuan temple walls and are part of the 2 meter high intertidal range that spans all the way to the Khafra enclosure. These blocks are extensively eroded showing intertidal notches that are due to wave mechanics and sea spray.
Credit text and pictures: Shérif El Morsi, 2010. copyright: AntoineGigal 2011