Mokattam Formation in the context of "Giza pyramid complex"

⭐ In the context of the Giza pyramid complex, the Mokattam Formation is most significantly known as…

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⭐ Core Definition: Mokattam Formation

The Mokattam Formation is a Middle Eocene-aged geological formation in northern Egypt. Consisting of nummulitic marine limestone outcropping across the Mokattam Hills, it has been extensively quarried from Ancient Egypt to the present day, and represents the source material for most of the famous archeological sites of Greater Cairo, most notably the Giza pyramid complex, the Great Sphinx, and much of Historic Cairo.

The age of the formation is thought to span from the late Lutetian to the Bartonian, depending on the member (Building Stone or Giushi). However, some authors treat the Giushi Member as its own geologic formation, which would restrict the Mokattam to just the Lutetian.

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👉 Mokattam Formation in the context of Giza pyramid complex

The Giza pyramid complex (also called the Giza necropolis) in Egypt is home to the Great Pyramid, the pyramid of Khafre, and the pyramid of Menkaure, along with their associated pyramid complexes and the Great Sphinx. All were built during the Fourth Dynasty of the Old Kingdom of ancient Egypt, between c. 2600 – c. 2500 BC. The site also includes several temples, cemeteries, and the remains of a workers' village.

The site is at the edge of the Western Desert, approximately 9 km (5.6 mi) west of the Nile River in the city of Giza, and about 13 km (8.1 mi) southwest of the city centre of Cairo. It forms the northernmost part of the 16,000 ha (160 km; 62 sq mi) Pyramid Fields of the Memphis and its Necropolis UNESCO World Heritage Site, inscribed in 1979. The pyramid fields include the Abusir, Saqqara, and Dahshur pyramid complexes, which were all built in the vicinity of Egypt's ancient capital of Memphis. Further Old Kingdom pyramid fields were located at the sites Abu Rawash, Zawyet El Aryan, and Meidum. Most of the limestone used to build the pyramids originates from the underlying Mokattam Formation.

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Mokattam Formation in the context of Great Sphinx of Giza

The Great Sphinx of Giza is a limestone statue of a reclining sphinx, a mythical creature with the head of a human and the body of a lion.

The monument was sculpted from the limestone bedrock of the Eocene-aged Mokattam Formation and faces east on the Giza Plateau, on the west bank of the Nile in Giza, Egypt. The oldest known monumental sculpture in Egypt, the Sphinx is part of the Memphite Necropolis and is a UNESCO World Heritage Site.

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Mokattam Formation in the context of Great Sphinx

The Great Sphinx of Giza is a limestone statue of a reclining sphinx, a mythical creature with the head of a human and the body of a lion. The monument was sculpted from the limestone bedrock of the Eocene-aged Mokattam Formation and faces east on the Giza Plateau, on the west bank of the Nile in Giza, Egypt. The oldest known monumental sculpture in Egypt, the Sphinx is part of the Memphite Necropolis and is a UNESCO World Heritage Site.

Archaeological evidence suggests the Sphinx was created by Egyptians of the Old Kingdom during the reign of Khufu (c. 2590–2566 BC) or Khafre (c. 2558–2532 BC). Scholars and Egyptologists believe the face of the Sphinx was carved to represent either the pharaoh Khufu or one of his sons, pharaohs Djedefre and Khafre, but a consensus has not been reached and the person(s) in whose likeness the Sphinx was carved remains in dispute.

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Mokattam Formation in the context of Tura limestone

Tura (Egyptian Arabic: طرة Tora  IPA: [ˈtˤoɾˤɑ], Coptic: ⲧⲣⲱⲁ, Ancient Greek: Τρωια or Τρωη) was the primary quarry for limestone in ancient Egypt. The site, which was known by the ancient Egyptians as Troyu or Royu, is located about halfway between modern-day Cairo and Helwan. Its ancient Egyptian name was misinterpreted by the ancient Greek geographer Strabo, who thought it meant it was inhabited by Trojans, thus the Hellenistic city was named Troia. The site is located by the modern town of Tora in the Cairo Governorate.

The limestone from the quarry is thought to be part of the Mokattam Formation, which was deposited during the late Lutetian stage of the Eocene epoch, about 42 million years. Some fossil fish species have been described from the quarry.

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