Lapis lazuli

Not to be confused with Lazulite.

For the Fabergé egg, see Lapis Lazuli (Fabergé egg).

"Lazuli" redirects here. For other uses, see Lazuli (disambiguation).

"Lapis" redirects here. For other uses, see Lapis (disambiguation).

Lapis lazuli

Metamorphic rock
Lapis lazuli in its natural state, with pyrite inclusions (specimen from Afghanistan)
Composition
Primary	Lazurite
Secondary	A mixture of other minerals, often including pyrite

Lapis lazuli (UK: /ˌlæpɪs ˈlæz(j)ʊli, ˈlæʒʊ-, -ˌli/; US: /ˈlæz(j)əli, ˈlæʒə-, -ˌli/), or lapis for short, is a deep-blue metamorphic rock used as a semi-precious stone that has been prized since antiquity for its intense color. Originating from the Persian word for the gem, lāžward, lapis lazuli is a rock composed primarily of the minerals lazurite, pyrite and calcite. As early as the 7th millennium BC, lapis lazuli was mined in the Sar-i Sang mines, in Shortugai, and in other mines in Badakhshan province in modern northeast Afghanistan. Lapis lazuli artifacts, dated to 7570 BC, have been found at Bhirrana, which is the oldest site of Indus Valley civilisation. Lapis was highly valued by the Indus Valley Civilisation (3300–1900 BC). Lapis beads have been found at Neolithic burials in Mehrgarh, the Caucasus, and as far away as Mauritania. It was used in the funeral mask of Tutankhamun (1341–1323 BC).

By the end of the Middle Ages, lapis lazuli began to be exported to Europe, where it was ground into powder and made into the pigment ultramarine. Ultramarine was used by some of the most important artists of the Renaissance and Baroque, including Masaccio, Perugino, Titian and Vermeer, and was often reserved for the clothing of the central figures of their paintings, especially the Virgin Mary. Ultramarine has also been found in dental tartar of medieval nuns and scribes, perhaps as a result of licking their painting brushes while producing medieval texts and manuscripts.

History

Excavations from Tepe Gawra show that Lapis lazuli was introduced to Mesopotamia approximately in the late Ubaid period, c. 4900–4000 BCE. A traditional understanding was that the lapis was mined some fifteen hundred miles to the east – in Badakhshan. Indeed, the Persian لاژورد lāžavard/lāževard, also written لاجورد lājevard, is commonly interpreted as having an origin in a local place name.

From the Persian, the Arabic لازورد lāzaward is the etymological source of both the English word azure (via Old French azur) and Medieval Latin lazulum, which came to mean 'heaven' or 'sky'. To disambiguate, lapis lazulī ("stone of lazulum") was used to refer to the stone itself, and is the term ultimately imported into Middle English. Lazulum is etymologically related to the color blue, and used as a root for the word for blue in several languages, including Spanish and Portuguese azul.

Mines in northeast Afghanistan continue to be a major source of lapis lazuli. Important amounts are also produced from mines west of Lake Baikal in Russia, and in the Andes mountains in Chile which is the source that the Inca used to carve artifacts and jewelry. Smaller quantities are mined in Pakistan, Italy, Mongolia, the United States, and Canada.

Science and uses

Composition

The most important mineral component of lapis lazuli is lazurite (25% to 40%), a blue feldspathoid silicate mineral of the sodalite family, with the formula (Na,Ca)
₈(AlSiO
₄)
₆(S,SO
₄,Cl)
_1–2. Most lapis lazuli also contains calcite (white), and pyrite (metallic yellow). Some samples of lapis lazuli contain augite, diopside, enstatite, mica, hauynite, hornblende, nosean, and sulfur-rich löllingite geyerite.

Lapis lazuli usually occurs in crystalline marble as a result of contact metamorphism.

Color

Lapis lazuli seen through a microscope (x240 magnification)

The intense blue color is due to the presence of the trisulfur radical anion (S^•−
₃) in the crystal. The presence of disulfur (S^•−
₂) and tetrasulfur (S^•−
₄) radicals can shift the color towards yellow or red, respectively. These radical anions substitute for the chloride anions within the sodalite structure. The S^•−
₃ radical anion exhibits a visible absorption band in the range 595–620 nm with high molar absorptivity, leading to its bright blue color.

Sources

Lapis lazuli is found in limestone in the Kokcha River valley of Badakhshan province in north-eastern Afghanistan, where the Sar-i Sang mine deposits have been worked for more than 6,000 years. Afghanistan was the source of lapis for the ancient Persian, Egyptian and Mesopotamian civilizations, as well as the later Greeks and Romans. Ancient Egyptians obtained the material through trade with Mesopotamians, as part of Egypt–Mesopotamia relations. During the height of the Indus Valley civilisation, approximately 2000 BC, the Harappan colony, now known as Shortugai, was established near the lapis mines.

In addition to the Afghan deposits, lapis is also extracted in the Andes (near Ovalle, Chile); and to the west of Lake Baikal in Siberia, Russia, at the Tultui lazurite deposit. It is mined in smaller amounts in Angola, Argentina, Burma, Pakistan, Canada, Italy, India, and in the United States in California and Colorado.

Uses and substitutes

Lapis takes an excellent polish and can be made into jewellery, carvings, boxes, mosaics, ornaments, small statues, and vases. Interior items and finishing buildings can be also made with lapis. During the Renaissance, lapis was ground and processed to make the pigment ultramarine for use in frescoes and oil painting. Its usage as a pigment in oil paint largely ended during the early 19th century, when a chemically identical synthetic variety became available.

Lapis lazuli is commercially synthesized or simulated by the Gillson process, which is used to make artificial ultramarine and hydrous zinc phosphates. Spinel or sodalite, or dyed jasper or howlite, can be substituted for lapis.

• 
  Crystals of lazurite (the main mineral in lapis lazuli) from the Sar-i Sang Mining District in Afghanistan
• 
  A polished block of lapis lazuli
• 
  Natural ultramarine pigment made from ground lapis lazuli. During the Middle Ages and Renaissance it was the most expensive pigment available (gold being second) and was often reserved for depicting the robes of Angels or the Virgin Mary
• 
  19th-century lapis lazuli and diamond pendant

History and art

In the ancient world

Further information: Art of ancient Egypt § Lapis lazuli

Ancient Egyptian cult image of Ptah; 945–600 BC; lapis lazuli; height of the figure: 5.2 cm, height of the dais: 0.4 cm; Metropolitan Museum of Art (New York City)

Lapis lazuli has been mined in Afghanistan and exported to the Mediterranean world and South Asia since the Neolithic age, along the ancient trade route between Afghanistan and the Indus Valley dating to the 7th millennium BC. Quantities of these beads have also been found at 4th millennium BC settlements in Northern Mesopotamia, and at the Bronze Age site of Shahr-e Sukhteh in southeast Iran (3rd millennium BC). A dagger with a lapis handle, a bowl inlaid with lapis, amulets, beads, and inlays representing eyebrows and beards, were found in the Royal Tombs of the Sumerian city-state of Ur from the 3rd millennium BC.

Lapis was also used in ancient Persia, Mesopotamia by the Akkadians, Assyrians, and Babylonians for seals and jewelry. It is mentioned several times in the Mesopotamian poem, the Epic of Gilgamesh (17th–18th century BC), one of the oldest known works of literature. The Statue of Ebih-Il, a 3rd millennium BC statue found in the ancient city-state of Mari in modern-day Syria, now in the Louvre, uses lapis lazuli inlays for the irises of the eyes.

In ancient Egypt, lapis lazuli was a favorite stone for amulets and ornaments such as scarabs. Lapis jewellery has been found at excavations of the Predynastic Egyptian site Naqada (3300–3100 BC). At Karnak, the relief carvings of Thutmose III (1479–1429 BC) show fragments and barrel-shaped pieces of lapis lazuli being delivered to him as tribute. Powdered lapis was used as eyeshadow by Cleopatra.

Jewelry made of lapis lazuli has also been found at Mycenae attesting to relations between the Myceneans and the developed civilizations of Egypt and the East.

Pliny the Elder wrote that lapis lazuli is "opaque and sprinkled with specks of gold". Because the stone combines the blue of the heavens and golden glitter of the sun, it was emblematic of success in the old Jewish tradition. In the early Christian tradition lapis lazuli was regarded as the stone of Virgin Mary.

In late classical times and as late as the Middle Ages, lapis lazuli was often called sapphire (sapphirus in Latin, sappir in Hebrew), though it had little to do with the stone today known as the blue corundum variety sapphire. In his book on stones, the Greek scientist Theophrastus described "the sapphirus, which is speckled with gold," a description which matches lapis lazuli.

Girl with a Pearl Earring by Vermeer

There are many references to "sapphire" in the Old Testament, but most scholars agree that, since sapphire was not known before the Roman Empire, they most likely are references to lapis lazuli. For instance, Exodus 24:10: "And they saw the God of Israel, and there was under his feet as it were a paved work of a sapphire stone..." (KJV). The words used in the Latin Vulgate Bible in this citation are "quasi opus lapidis sapphirini", the terms for lapis lazuli. Modern translations of the Bible, such as the New Living Translation Second Edition, refer to lapis lazuli in most instances instead of sapphire.

Vermeer

Johannes Vermeer used lapis lazuli paint, in the Girl with a Pearl Earring painting.

Yeats

The poet, William Butler Yeats, describes a figurine of sculpted lapis lazuli in a poem entitled "Lapis Lazuli". The sculpture of three men from China, a bird, and a musical instrument serves in the poem as a reminder of "gaiety" in the face of tragedy.

Gallery

• 
  A bovine with eyes decorated with lapis lazuli. Fertile Crescent, Sumerian, 889-853 B.C.
• 
  Sumerian bald clean-shaven male worshipper head, 2600–2500 BC; gypsum, shell, lapis lazuli and bitumen; from Nippur (Iraq); Museum of the Institute for the Study of Ancient Cultures (Chicago)
• 
  Sumerian necklace beads; 2600–2500 BC; gold and lapis lazuli; length: 54 cm; Metropolitan Museum of Art (New York City)
• 
  Sumerian necklace; 2600–2500 BC; gold and lapis lazuli; length: 22.5 cm; from the Royal Cemetery at Ur (Iraq); Metropolitan Museum of Art
• 
  Ancient Egyptian scarab finger ring; 1850–1750 BC; lapis lazuli scarab set in gold plate and on a gold wire ring lapis-lazuli; diameter: 2.5 cm, the scarab: 1.8 cm; Metropolitan Museum of Art
• 
  Neo-Babylonian conical seal; 7th–6th century BC; lapis lazuli; height: 2.7 cm, diameter: 2.1 cm; Metropolitan Museum of Art
• 
  Ancient Egyptian plaque with an Eye of Horus; 664–332 BC; lapis lazuli; length: 1.8 cm, width: 1.6 cm; Metropolitan Museum of Art
• 
  Greek or Roman ring stone; lapis lazuli; 2.1 x 1.6 x 0.3 cm; Metropolitan Museum of Art
• 
  Roman bead ornament; gold and lapis lazuli; 3 × 1.8 × 0.5 cm; Metropolitan Museum of Art
• 
  20th century silver ring with polished lapis oval; 2 x 2.4 x 1 cm
• 
  Elephant carved from lapis lazuli. Length 7 cm.
• 
  Large lapis lazuli specimen from Afghanistan's Hindu Kush mountains. National Museum of Natural History (Washington, D.C.)

See also

• Dvārakā–Kamboja route
• Hauyne – Silicate mineral
• Lapis armenus – Precious stone resembling lapis lazuli
• Sar-i Sang – town in Badakhshan Province, AfghanistanPages displaying wikidata descriptions as a fallback
• Shades of blue – Variety of the color blue
• Ultramarine – Deep blue purple color pigment which was originally made with ground lapis lazuli

References

Bibliography

• Bakhtiar, Lailee McNair, Afghanistan's Blue Treasure Lapis Lazuli, Front Porch Publishing, 2011, ISBN 978-0615573700
• Bariand, Pierre, "Lapis Lazuli", Mineral Digest, Vol 4 Winter 1972.
• Bowersox, Gary W.; Chamberlin, Bonita E. (1995). Gemstones of Afghanistan. Tucson, AZ: Geoscience Press.
• Herrmann, Georgina, "Lapis Lazuli: The Early Phases of Its Trade", Oxford University Dissertation, 1966.
• Korzhinskij, D. S., "Gisements bimetasomatiques de philogophite et de lazurite de l'Archen du pribajkale", Traduction par Mr. Jean Sagarzky-B.R.G.M., 1944.
• Lapparent A. F., Bariand, P. et Blaise, J., "Une visite au gisement de lapis lazuli de Sar-e-Sang du Hindu Kouch, Afghanistan," C.R. Somm.S.G.P.p. 30, 1964.
• Oldershaw, Cally (2003). Firefly Guide to Gems. Toronto: Firefly Books..
• Wise, Richard W., Secrets of the Gem Trade: The Connoisseur's Guide to Precious Gemstones, 2016 ISBN 9780972822329
• Wyart J. Bariand P, Filippi J., "Le Lapis Lazuli de Sar-e-SAng", Revue de Geographie Physique et de Geologie Dynamique (2) Vol. XIV Pasc. 4 pp. 443–448, Paris, 1972.

External links

• Lapis lazuli at Gemstone.org
• Documentation from online course produced by University of California at Berkeley
• Lapislazuli: Occurrence, Mining and Market Potential of a blue Mineral Pigment
• "Lapis Lazuli" . The New Student's Reference Work . 1914.
• "Why a Medieval Woman Had Lapis Lazuli Hidden in Her Teeth", The Atlantic, January 2019
• Lapis Lazuli birthstone virtues and story at birthstone.guide