Amethyst

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Amethyst
Amatista Laye 2.jpg
Amethyst cluster from Artigas, Uruguay
General
Category Silicate mineral
Formula
(repeating unit)
Silica (silicon dioxide, Si O 2)
Crystal system Trigonal
Crystal class Trapezohedral (32)
Space group P3221 (no. 154)
Identification
ColorPurple, violet, dark purple
Crystal habit 6 sided prism ending in 6 sided pyramid (typical)
Twinning Dauphine law, Brazil law, and Japan law
Cleavage None
Fracture Conchoidal
Mohs scale hardness7 (lower in impure varieties)
Luster Vitreous/glassy
Streak White
Diaphaneity Transparent to translucent
Specific gravity 2.65 constant; variable in impure varieties
Optical propertiesUniaxial (+)
Refractive index nω = 1.543–1.553
nε = 1.552–1.554
Birefringence +0.009 (B-G interval)
Pleochroism Weak to moderate purple/reddish purple
Melting point 1650±75 °C
Solubility Insoluble in common solvents
Other characteristics Piezoelectric

Amethyst is a violet variety of quartz. The name comes from the Koine Greek αμέθυστος amethystos from α-a-, "not" and μεθύσκω (Ancient Greek) methysko / μεθώmetho (Modern Greek), "intoxicate", a reference to the belief that the stone protected its owner from drunkenness. [1] Ancient Greeks wore amethyst and carved drinking vessels from it in the belief that it would prevent intoxication.

Contents

Amethyst, a semiprecious stone, is often used in jewelry.

Structure

Amethyst is a purple variety of quartz (SiO
2
) and owes its violet color to irradiation, impurities of iron (Fe3+
) and in some cases other transition metals, and the presence of other trace elements, which result in complex crystal lattice substitutions. [2] [3] [4] The irradiation causes the iron Fe3+
ions that replace Si in the lattice to lose an electron and form a [FeO
4
]
0 color center. [5] Amethyst is a three-dimensional network of tetrahedra where the silicon atoms are in the center and are surrounded by four oxygen atoms located at the vertices of a tetrahedron. This structure is quite rigid and results in quartz's hardness and resistance to weathering. The hardness of the mineral is the same as quartz, thus making it suitable for use in jewelry.

Hue and tone

Amethyst occurs in primary hues from a light lavender or pale violet to a deep purple. Amethyst may exhibit one or both secondary hues, red and blue. [6] High-quality amethyst can be found in Siberia, Sri Lanka, Brazil, Uruguay, and the Far East. The ideal grade, called "Deep Siberian", has a primary purple hue of around 75–80%, with 15–20% blue and (depending on the light source) red secondary hues. [7] "Rose de France" is defined by its markedly light shade of the purple, reminiscent of a lavender / lilac shade. These pale colors were once considered undesirable, but have recently become popular due to intensive marketing. [8]

Green quartz is sometimes called green amethyst; the scientific name is prasiolite. [9] Other names for green quartz are vermarine and lime citrine.

Amethyst frequently shows color zoning, with the most intense color typically found at the crystal terminations. One of gem cutters' tasks is to make a finished product with even color. Sometimes, only a thin layer of a natural, uncut amethyst is violet colored, or the color is very uneven. The uncut gem may have only a small portion that is suitable for faceting. [10] [11]

Geode Reference -25.jpg
Natural purple/violet amethyst
Citrine amethysee.jpg
Heat-treated amethyst
Pink amethyst 1.jpg
Natural pink amethyst

The color of amethyst has been demonstrated to result from substitution by irradiation of trivalent iron (Fe3+) for silicon in the structure, [4] [12] in the presence of trace elements of large ionic radius, [3] and to a certain extent, the amethyst color can naturally result from displacement of transition elements even if the iron concentration is low. Natural amethyst is dichroic in reddish violet and bluish violet, [4] but when heated, turns yellow-orange, yellow-brown, or dark brownish and may resemble citrine, [13] but loses its dichroism, unlike genuine citrine. When partially heated, amethyst can result in ametrine.

Amethyst can fade in tone if overexposed to light sources, and can be artificially darkened with adequate irradiation. [4] It does not fluoresce under either short-wave or long-wave UV light.

Geographic distribution

Amethyst is found in many locations around the world. Between 2000 and 2010, the greatest production was from Marabá and Pau d'Arco, Pará, and the Paraná Basin, Rio Grande do Sul, Brazil; Sandoval, Santa Cruz, Bolivia; Artigas, Uruguay; Kalomo, Zambia; and Thunder Bay, Ontario. Lesser amounts are found in many other locations in Africa, Brazil, Spain, Argentina, Russia, Afghanistan, South Korea, Mexico, and the United States. [14]

Main amethyst-producing countries Quartz gisements.jpg
Main amethyst-producing countries

Amethyst is produced in abundance in the state of Rio Grande do Sul in Brazil where it occurs in large geodes within volcanic rocks. [15] [16] [17] [18]

Many of the hollow agates of southwestern Brazil and Uruguay contain a crop of amethyst crystals in the interior. Artigas, Uruguay and neighboring Brazilian state Rio Grande do Sul are large world producers, with lesser quantities mined in Minas Gerais and Bahia states. [14]

An amethyst geode that formed when large crystals grew in open spaces inside the rock Geode di quarzo ametista dal rio grande do sul, brasile.JPG
An amethyst geode that formed when large crystals grew in open spaces inside the rock

The largest amethyst geode found as of 2007 was the Empress of Uruguay, found in Artigas, Uruguay in 2007. It stands at a height of 3.27 meters, lies open along its length, and weighs 2.5 tons.

Amethyst is also found and mined in South Korea. [19] The large opencast amethyst vein at Maissau, Lower Austria, was historically important, [1] but is no longer included among significant producers. [14] Much fine amethyst comes from Russia, especially near Mursinka in the Ekaterinburg district, where it occurs in drusy cavities in granitic rocks. [1] [14] Amethyst was historically mined in many localities in south India, [1] though these are no longer significant producers. [14] One of the largest global amethyst producers is Zambia in southern Africa, with an annual production around 1000 tons. [20]

Amethyst occurs at many localities in the United States. The most important production is at Four Peaks, Gila and Maricopa Counties, Arizona, and Jackson's Crossroads, Wilkes County, Georgia. [14]

Smaller occurrences have been reported in the Red Feather Lakes, near Fort Collins, Colorado; Amethyst Mountain, Texas; Yellowstone National Park; Delaware County, Pennsylvania; Haywood County, North Carolina; Deer Hill and Stow, Maine, and in the Lake Superior region of Minnesota, Wisconsin, and Michigan. [1]

Amethyst is relatively common in the Canadian provinces of Ontario and Nova Scotia. The largest amethyst mine in North America is located in Thunder Bay, Ontario. [14]

Amethyst is the official state gemstone of South Carolina. Several South Carolina amethysts are on display at the Smithsonian Museum of Natural History. [21]

History

Intaglio Caracalla Cdm Paris Chab2101.jpg
Roman intaglio engraved gem of Caracalla in amethyst, once in the Treasury of Sainte-Chapelle
Uninscribed amethyst scarab at the center of a string of amethyst ball beads. Middle Kingdom. From Egypt. The Petrie Museum of Egyptian Archaeology, London.jpg
Uninscribed amethyst scarab at the center of a string of amethyst ball beads from Egypt

Amethyst was used as a gemstone by the ancient Egyptians and was largely employed in antiquity for intaglio engraved gems. [22]

The ancient Greeks believed amethyst gems could prevent intoxication, [23] while medieval European soldiers wore amethyst amulets as protection in battle in the belief that amethysts heal people and keep them cool-headed. [24] (p 77) Beads of amethyst were found in Anglo-Saxon graves in England. [25] Anglican bishops wear an episcopal ring often set with an amethyst, an allusion to the description of the Apostles as "not drunk" at Pentecost in Acts 2:15. [26]

A large geode, or "amethyst-grotto", from near Santa Cruz in southern Brazil was presented at a 1902 exhibition in Düsseldorf, Germany. [1]

The meaning of amethyst varies from time to time and culture, which is why amethyst has different meanings in Feng Shui and focuses on increasing wealth. In ancient China, it was also used as a powerful tool to remove negative energies and drive away the hazards of daily life.[ self-published source? ]

Synthetic amethyst

Synthetic (laboratory-grown) amethyst is produced by a synthesis method called hydrothermal growth, which grows the crystals inside a high-pressure autoclave.

Synthetic amethyst is made to imitate the best quality amethyst. Its chemical and physical properties are the same as those of natural amethyst, and it cannot be differentiated with absolute certainty without advanced gemmological testing (which is often cost-prohibitive). One test based on "Brazil law twinning" (a form of quartz twinning where right- and left-hand quartz structures are combined in a single crystal [27] ) can be used to identify most synthetic amethyst rather easily. Synthesizing twinned amethyst is possible, but this type is not available in large quantities in the market. [7]

Treated amethyst is produced by gamma ray, X-ray, or electron-beam irradiation of clear quartz (rock crystal), which has been first doped with ferric impurities. Exposure to heat partially cancels the irradiation effects and amethyst generally becomes yellow or even green. Much of the citrine, cairngorm, or yellow quartz of jewelry is said to be merely "burnt amethyst". [1] [28]

Cultural history

Ancient Greece

Emerald cut amethyst Amethyst close cropped.jpg
Emerald cut amethyst

The Greek word amethystos may be translated as "not drunken", from Greek a-, "not" + methustos, "intoxicated". Amethyst was considered to be a strong antidote against drunkenness. [lower-alpha 1] {{efn| In his poem "L'Amethyste, ou les Amours de Bacchus et d'Amethyste" (Amethyst or the loves of Bacchus and Amethyste), the French poet Rémy Belleau (1528–1577) invented a myth in which Bacchus, the god of intoxication, of wine, and grapes was pursuing a maiden named Amethyste, who refused his affections. Amethyste prayed to the gods to remain chaste, a prayer which the chaste goddess Diana answered, transforming her into a white stone. Humbled by Amethyste's desire to remain chaste, Bacchus poured wine over the stone as an offering, dyeing the crystals purple. [lower-alpha 2] [24] (p 58–59)


Variations of the story include that Dionysus had been insulted by a mortal and swore to slay the next mortal who crossed his path, creating fierce tigers to carry out his wrath. The mortal turned out to be a beautiful young woman, Amethystos, who was on her way to pay tribute to Artemis. Her life was spared by Artemis, who transformed the maiden into a statue of pure crystalline quartz to protect her from the brutal claws. Dionysus wept tears of wine in remorse for his action at the sight of the beautiful statue. The god's tears then stained the quartz purple. [34]

This myth and its variations are not found in classical sources. However, the goddess Rhea does present Dionysus with an amethyst stone to preserve the wine-drinker's sanity in historical text. [35]

Other cultural associations

Tibetans consider amethyst sacred to the Buddha and make prayer beads from it. [36] [ full citation needed ] Amethyst is considered the birthstone of February. [37] In the Middle Ages, it was considered a symbol of royalty and used to decorate English regalia. [37] In the Old World, amethyst was considered one of the cardinal gems, in that it was one of the five gemstones considered precious above all others, until large deposits were found in Brazil. [38]

Value

2012 Tucson 22nd Street Show 18.JPG
2012 Tucson Gem & Mineral Show 85.JPG
Amethyst geodes displayed at the 2012 Tucson Gem & Mineral Show

Until the 18th century, amethyst was included in the cardinal, or most valuable, gemstones (along with diamond, sapphire, ruby, and emerald), but since the discovery of extensive deposits in locations such as Brazil, it has lost most of its value. [38] It is now considered a semiprecious stone. [39]

Collectors look for depth of color, possibly with red flashes if cut conventionally. [40] As amethyst is readily available in large structures, the value of the gem is not primarily defined by carat weight. This is different from most gemstones, since the carat weight typically exponentially increases the value of the stone. The biggest factor in the value of amethyst is the color displayed. [41]

The highest-grade amethyst (called deep Russian) is exceptionally rare. When one is found, its value is dependent on the demand of collectors; however, the highest-grade sapphires or rubies are still orders of magnitude more expensive than amethyst. [7]

Handling and care

The most suitable setting for gem amethyst is a prong or a bezel setting. The channel method must be used with caution. [42]

Amethyst has a good hardness, and handling it with proper care will prevent any damage to the stone. Amethyst is sensitive to strong heat and may lose or change its colour when exposed to prolonged heat or light. Polishing the stone or cleaning it by ultrasonic or steamer must be done with caution. [42]

Footnotes

  1. The earliest reference to amethyst as a symbol of sobriety is in a poem by Asclepiades of Samos (born c.320 BCE). [29]
    An epigram by Plato the Younger also mentions amethyst in connection with drinking: "The stone is an amethyst; but I, the tipler Dionysus, say, "Let it either persuade me to be sober, or let it learn to get drunk." [30]
    Pliny says about amethysts: "The falsehoods of the magicians would persuade us that these stones are preventive of inebriety, and that it is from this that they have derived their name." [31] which is why wine goblets were often carved from it. [32]
  2. The "myth" of Amethyste and Bacchus was invented by the French poet Remy Belleau (1528–1577). [33]

See also

Amethystre sceptre2.jpg  Mineralsportal

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References

  1. 1 2 3 4 5 6 7 Wikisource-logo.svg One or more of the preceding sentences incorporates text from a publication now in the public domain : Rudler, Frederick William (1911). "Amethyst". In Chisholm, Hugh (ed.). Encyclopædia Britannica . Vol. 1 (11th ed.). Cambridge University Press. p. 852.
  2. Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth–Heinemann. ISBN   0080379419.
  3. 1 2 Lameiras, Fernando S.; Nunes, Eduardo H.M.; Vasconcelos, Wander L. (2009). "Infrared and chemical characterization of natural amethysts and prasiolites colored by irradiation". Materials Research. 12 (3): 315–320. doi: 10.1590/S1516-14392009000300011 .
  4. 1 2 3 4 O'Donoghue, Michael (2006). Gems (6th ed.). Butterworth-Heinemann. ISBN   978-0-7506-5856-0.
  5. Lehmann; Moore (1966). "Amethyst". mindat.org.
  6. "Amethyst: The world's most popular purple gemstone". geology.com. Retrieved 29 August 2017.
  7. 1 2 3 Wise, Richard W. (2005). Secrets of the Gem Trade: The connoisseurs' guide to precious gemstones. Lenox, MA: Brunswick House Press. ISBN   0-9728223-8-0.
  8. Arem, Joel E.; Clark, Donald; Smigel, Barbara. "Amethyst: Value, price, and jewelry information". gemsociety.org. International Gem Society (IGS). Retrieved 20 April 2021.
  9. "Prasiolite gemstone information". gemdat.org. Retrieved 19 April 2018.
  10. Lowell, J.; Koivula, J.I. (2004). "Amethyst from four peaks, Arizona" (PDF). Gems & Gemology . 40 (3): 230–238. doi:10.5741/GEMS.40.3.230. Archived (PDF) from the original on 9 October 2022. Retrieved 20 April 2021.
  11. Troilo, Fabrizio; el Harfi, Abdelghani; Mouaddib, Salahaddine; Bitarello, Erica; Costa, Emanuele (1 May 2015). "Amethyst from Boudi, Morocco". Gems & Gemology. 51 (1): 32–40. doi:10.5741/GEMS.51.1.32.
  12. Rossman, George R. (1994). "Chapter 13. Colored varieties of the silica minerals". In Heaney, Peter J.; Prewitt, Charles T.; Gibbs, Gerald V. (eds.). Silica: Physical behavior, geochemistry, and materials applications. Reviews in Mineralogy. Vol. 29. Mineralogical Society of America / Mineralogical Magazine. pp. 433–468. Bibcode:1996MinM...60..390H. doi:10.1180/minmag.1996.060.399.16. ISBN   978-0-939950-35-5. S2CID   201093227.
  13. "Amethyst". Mindat.org.
  14. 1 2 3 4 5 6 7 Shigley, J.E.; Laurs, B.M.; Janse, A.J.A.; Elen, S.; Dirlam, D.M. (2010). "Gem Localities of the 2000s" (PDF). Gems & Gemology . 46 (3): 188–216. doi:10.5741/GEMS.46.3.188. Archived (PDF) from the original on 9 October 2022. Retrieved 20 April 2021.
  15. "Serviço Geológico do Brasil". cprm.gov.br. Retrieved 31 January 2022.
  16. "Os alemães e as pedras preciosas gaúchas". GZH (in Brazilian Portuguese). 27 February 2018. Retrieved 31 January 2022.
  17. "Maior pedra de água-marinha é brasileira e ficará exposta nos EUA". Ciência e Saúde (g1.globo.com/ciencia-e-saude) (in Brazilian Portuguese). 7 December 2012. da EFE. Retrieved 31 January 2022.
  18. "Pedras de ametista são atrativos para turistas em cidade no Norte do RS". g1.globo.com. Nossa Terra 2013 (in Brazilian Portuguese). 4 July 2013. Do G1 RS. Retrieved 31 January 2022.
  19. Yang, K.H.; Yun, S.H.; Lee, J.D. (2001). "A fluid inclusion study of an amethyst deposit in the Cretaceous Kyongsang Basin, South Korea". Mineralogical Magazine . 65 (4): 477–487. Bibcode:2001MinM...65..477Y. doi:10.1180/002646101750377515. S2CID   129368598 . Retrieved 20 April 2021.
  20. Anckar, B. (2006). "Amethyst Mining in Zambia". Gems & Gemology . 42 (3): 112–113.
  21. "South Carolina state gemstone - amethyst". Sciway.net. 24 June 1969. Retrieved 4 February 2016.
  22. Castellani, Augosto (1871). Gems, Notes, and Extracts. London, UK: Bell and Daldy. p. 34. ISBN   1-141-06174-0. — Castellani was a 19th century Italian jeweler, now famous
  23. Smith, Marcell N. (1913). Diamonds, Pearls, and Precious Stones. Boston, MA: Griffith Stillings Press. p. 74.
  24. 1 2 Kunz, G.F. (1913). Curious Lore of Precious Stones. Philadelphia, PA / London, UK: Lippincott Company. p. 58–59, 77.
  25. Lapidge, Michael, ed. (2000). The Blackwell Encyclopaedia of Anglo-Saxon England. Wiley. p. 261. ISBN   0631224920.
  26. Bays, P. (2012). This Anglican Church of Ours. Woodlake Books. p. 136. ISBN   9781770644397. name=google
  27. "twinning crystals". Quartz Page (quartzpage.de).
  28. Michael O'Donoghue (1997). Synthetic, Imitation, and Treated Gemstones. Taylor & Francis. pp. 124–125. ISBN   978-0-7506-3173-0.
  29. Asclepiades of Samos (1920). "XXX. Kleopatra's Ring". The Windflowers of Asklepiades and the Poems of Poseidippos. Translated by Storer, Edward. London, UK: Egoist Press. p. 14.
  30. Burges, George; et al., eds. (1881). The Greek Anthology. London, UK: George Bell and Sons. p.  369.
  31. Pliny the Elder. "Book 37, Chapter 40". Natural History.
  32. Federman, David (2012). Modern Jeweler's Consumer Guide to Colored Gemstones. Springer Science & Business Media. p. 28. ISBN   978-1-4684-6488-7.
  33. Belleau, Remy (1576). "L'Amethyste, ou les Amours de Bacchus et d'Amethyste". Les Amours et Nouveaux Eschanges des Pierres Precieuses: Vertus & Proprietez d'icelles[The loves and new transformations of the precious stones: Their virtues and properties] (in French). Paris, FR: Mamert Patisson. pp.  4–6. — Belleau's collection of poems
  34. "Amethyst". Gemstone.org.
  35. Nonnus, Dionysiaca, 12. 380
  36. Clark, Carol. Tropical Gemstones. p. 52.
  37. 1 2 "February birthstone: Amethyst". American Gem Society (americangemsociety.org). 12 January 2016. Retrieved 4 February 2016.
  38. 1 2 Geary, T.F.; Whalen, D. (2008). The Illustrated Bead Bible: Terms, tips & techniques. Sterling Pub. p. 69. ISBN   9781402723537. Archived from the original on 16 January 2021. Retrieved 19 July 2015.
  39. Souza, Tamires P.; Watte, Guilherme; Gusso, Alaíde M.; Souza, Rafaela; Moreira, José da S.; Knorst, Marli M. (June 2017). "Silicosis prevalence and risk factors in semi-precious stone mining in Brazil". American Journal of Industrial Medicine . 60 (6): 529–536. doi:10.1002/ajim.22719. PMID   28514023. S2CID   24375063.
  40. The Gemstone Book: Gemstones, organic substances, & artificial products — terminology & classification (PDF). The World Jewellery Confideration (CIBJO). 2011. Archived from the original (PDF) on 12 August 2012. Retrieved 27 June 2012.
  41. "Amethyst jewelry and gemstones information". International Gem Society (IGS). Retrieved 3 October 2014 via gemsociety.org.
  42. 1 2 Gemstone Durability Design to Display (PDF) (Report). Gemological Institute of America (GIA). Archived (PDF) from the original on 30 April 2019 via gia.edu.