Stone quarries of ancient Egypt

Gebel el Ahmar

Gebel el Ahmar is located near Cairo on the east bank of the Nile, near the suburb of Heliopolis. The name means Red Mountain. The site was in full production in the times of Amenhophis III, Akhenaton, Tutankhamon, and Ramses III. The quarry was directed by Huy, known as "Chief of the King's Works", and also by Hori. The quarry was active during the Pharonic period and is now largely destroyed in modern time.

Typical materials known from this site are:

• Red and brown silicified sandstone or quartzite

Some of the monuments known to come from this site are:

• The Colossi of Memnon

Mokattam Hills

The Mokattam hills are a site located near Memphis. The hills were quarried for limestone during the pharonic period.

Typical materials known from this site are:

• Mokattam limestone

Tura-Masara

Tura-Masara is located 12 km (7.5 mi) south of Cairo and spans 6 km (3.7 mi) of underground quarries along the eastern bank of the Nile. The Tura quarry and Masara quarry are often separated, viewed individually, but due to their proximity they are more appropriately recognized as one extended system. The quarries were active sometime during the Old Kingdom through the Late Period and remain partially destroyed in present day.

Typical materials known from this site are:

• High quality, fine-grained white limestone

Some of the monuments known to use materials from this site are:

• Casing stones for 4th-6th dynasty pyramids
• Memphite necropolis in the 12th dynasty

Umm es-Sawan

Umm es-Sawan is located on Gevel el-Qatrani, Faiyum, 20 km (12.4 mi) north-east of Wide el-Faras in the landscape of the Northern Faiyum Desert. The white gypsum from this site occurs in near-vertical veins that cross-cut the other stratigraphy. The quarry was active during the Pharonic period and remains largely intact.

Typical materials known from this site are:

• Fine-grained white gypsum or alabaster

Widan el-Faras

Widan el-Faras is located on Gebel el-Qatrani, Faiyum, 60 km (37 mi) southwest of Cairo in the Western Desert and is one of the oldest preserved hard-stone quarries sites. Widen el-Faras, literarily translates to "Ears of the Mare" and is named for the twin peaks located east of the quarry site. The quarry landscape of the Northern Faiyum Desert comprise both the Umm es-Sawan and Widan el-Faras basalt quarries, both heavily exploited for hardstone during the Old Kingdom pyramid age due to their proximity to the Nile Valley. The quarry was active between the Old Kingdom and Late Period. The ancient quarries have since been partially destroyed but Widen el-Faras continues to be a site for modern quarrying through the 20th century.

Typical materials known from this site are:

• Dark gray to black basalt
• Petrified wood
• Gypsum

Some of the monuments known to use materials from this site are:

• 4th and 5th dynasty mortuary temple walls and floors
• Blocks of basalt made up the floor of the funerary temple east of Khufu's Great Pyramid
• 11.5 km long, paved quarry road connecting Widan el-Faras and Qasr el-Sagha used basalt fragments from the quarry along with other materials such as limestone, sandstone, and petrified wood.

El Amarna

The El Amarna site is located a short distance from El Amarna.

Typical materials known from this site are:

• Alabaster

Gabal Abu Dukhan

The Gabal Abu Dukhan site, near modern Hurghada on Egypt's Red Sea coast, was particularly important for the Roman Empire. Pliny the Elder's Natural History stated that "imperial porphyry" was discovered at an isolated site in Egypt in 18 CE by a Roman legionary named Caius Cominius Leugas. The location of the site, known to the Romans as Mons Porphyrites, was lost for many centuries until rediscovered in the 19th century. It was the only source of imperial porphyry in antiquity. The quarry was active during the Greco-Roman period.

Typical materials known from this site are:

• Reddish-Purple porphyry with pale pink to white phenocrysts
• Greenish-black porphyry with pale green to white phenocrysts
• Black porphyry with pale green to mostly white phenocrysts

Some of the monuments known to come from this site are:

• The baptismal font in the Cathedral of Magdeburg, Germany.
• The porphyry togas of the busts of Roman Emperors
• Porphyry panels in the Pantheon
• The Portrait of the Four Tetrarchs

Koptos

Koptos is located in Wadi Rohanu.

Typical materials known from this site are:

• Black slate

Wadi Hammamat

Wadi Hammamat is a quarrying area located in the Eastern Desert of Egypt. This site is noted because it is described in the first ancient topographic map known, the Turin Papyrus Map, describing a quarrying expedition prepared for Ramesses IV. Inscriptions found at Wadi Hammamat describe quarry workers breaking blocks from the mountain and using a ramp to lower them to the ground when a monument was requested by the King. Wadi Hammamat was active through the Pharonic period into the Greco-Roman period and remains largely intact in modern time.

Typical materials known from this site are:

• Basalt
• Basanite
• Metagraywacke and metaconglomerate

Qurna

Qurna is located near Thebes. It was an active site during the reign of Amenhotep III.

Typical materials known from this site are:

• Limestone

El-Dibabiya

El-Dibabiya was a limestone quarry site at the southern end of the Eastern Desert in Egypt along the Nile. The quarry was active during the Old Kingdom and remained active into the Greco-Roman period in Egypt. The site remains largely intact.

Typical materials known from this site are:

• Limestone

Edfu

These quarries are located 8 km (5.0 mi) north of Edfu.

Some of the monuments known to come from this site are:

• Stone blocks used by the engineers of Septimius Severus to reconstruct the north Colossus of Memnon.

Gebel el-Silsila

Gebel el-Silsila or Gebel Silsileh is 64 km (40 mi) north of Aswan along the banks of the Nile. It was a very well known quarrying area throughout all of ancient Egypt due to the quality of the building stone quarried there. The site is a rich archaeological area, with temples cut directly in the hills. Examples include the rock temple of Horemheb on the west bank. Many of the monuments here bear inscriptions of Hatshepsut, Amenhotep II, Ramesses II, Merenptah, and Ramesses III. The quarries and the stone temples here are visible from boats on the Nile. The quarry was active sometime during the Old Kingdom through the Late Period and remains largely intact in modern time.

Typical materials known from this site are:

• Sandstone

Some of the monuments known to come from this site are:

• Temple of Horemheb

The quarries of Aswan

The quarries of Aswan are located along the Nile near the city of Aswan. There are a number of well-known sites: Shellal, consisting of northern and southern quarries within an area of about 20 km² (7.7 sq mi) on the west bank, and the islands of Elephantine and Seheil. One of the known directors of the Aswan sites was Hori during the reign of Ramses III. Great amounts of granite were quarried from Aswan at an extent only comparable to ancient Egypt's limestone and sandstone quarries. The quarry sites were active in the Old Kingdom through the Late Period, and continued to be active in the Greco-Roman period of Egypt. In the present days, the quarry area is to become an open-air museum.

Typical materials known from this site are:

• Coarse-grained pinkish to reddish granite
• Coarse-grained gray to black granodiorite
• Fined-grained pinkish to gray granite
• Black Dolerite

Some of the monuments known to come from this site are:

• Cleopatra's Needle
• The unfinished obelisk still on site, at the northern quarry
• The unfinished partly worked obelisk base, discovered in 2005
• The sarcophagus made from granite at the burial chambers of the Third Dynasty Pharaoh Djoser at Saqqara and the Fourth Dynasty Pharaoh Sneferu at Dahshur
• The Grand Gallery and the King's Chamber within the pyramid of Khufu as well as his granite block sarcophagus
• Sarcophagus and lowest layer of outer casing in the pyramid of Khafre at Giza, as well as a statue of Khafre all made of granite
• Burial chamber and lower layers of outer casing in the pyramid of Menkaure at Giza made of granite

Idahet

The site is located a few kilometres from Idahet, in barren desert terrain. It was abandoned during the Middle Kingdom.

Typical materials known from this site are:

• diorite

Other sites

Other important quarry sites include:

• Alabaster quarries at Hatnub
• Chephren's Gneiss Quarry
• Limestone quarries north of Cairo