The word "emerald" is derived (viaOld French:esmeraude andMiddle English:emeraude), fromVulgar Latin:esmaralda/esmaraldus, a variant ofLatinsmaragdus, which was viaAncient Greek:σμάραγδος (smáragdos; "green gem"). The Greek word may have a Semitic, Sanskrit or Persian origin.[4][5][6] According toWebster's Dictionary the term emerald was first used in the 14th century.[7]
Emeralds, like all coloredgemstones, are graded using four basic parameters known as "the fourCs":color,clarity,cut andcarat weight. Normally, in grading colored gemstones, color is by far the most important criterion. However, in the grading of emeralds, clarity is considered a close second. A fine emerald must possess not only a pure verdant greenhue as described below, but also a high degree oftransparency to be considered a top gemstone.[8]
This member of the beryl family ranks among the traditional "big four" precious gems along withdiamonds,rubies andsapphires.[9]
In the 1960s, the American jewelry industry changed the definition ofemerald to include the green vanadium-bearing beryl. As a result,vanadium emeralds purchased as emeralds in the United States are not recognized as such in the United Kingdom and Europe. In America, the distinction between traditional emeralds and the new vanadium kind is often reflected in the use of terms such as "Colombian emerald".[10]
Ingemology,[11] color is divided into three components:hue,saturation, andtone. Emeralds occur in hues ranging from yellow-green to blue-green, with the primary hue necessarily being green. Yellow and blue are the normal secondary hues found in emeralds. Only gems that are medium to dark in tone are considered emeralds; light-toned gems are known instead by the species namegreen beryl. The finest emeralds are approximately 75% tone on a scale where 0% tone is colorless and 100% is opaque black. In addition, a fine emerald will be saturated and have a hue that is bright (vivid). Gray is the normal saturation modifier or mask found in emeralds; a grayish-green hue is a dull-green hue.[8]
Brazilian emerald (grass-green variety of the mineral beryl) in a quartz-pegmatite matrix with typical hexagonal, prismatic crystals.[12]
Emeralds tend to have numerous inclusions and surface-breakingfissures. Unlike diamonds, where theloupe standard (i.e., 10× magnification) is used to grade clarity, emeralds are graded by eye. Thus, if an emerald has no visibleinclusions to the eye (assuming normal visual acuity) it is considered flawless. Stones that lack surface breaking fissures are extremely rare and therefore almost all emeralds are treated ("oiled", see below) to enhance the apparent clarity. The inclusions and fissures within an emerald are sometimes described asjardin (French forgarden), because of their mossy appearance.[13] Imperfections are unique for each emerald and can be used to identify a particular stone. Eye-clean stones of a vivid primary green hue (as described above), with no more than 15% of any secondary hue or combination (either blue or yellow) of a medium-dark tone, command the highest prices.[8] The relative non-uniformity motivates the cutting of emeralds incabochon form, rather than faceted shapes. Faceted emeralds are most commonly given an oval cut, or the signature emerald cut, a rectangular cut with facets around the top edge.
Most emeralds are oiled as part of the post-lapidary process, in order to fill in surface-reaching cracks so that clarity and stability are improved.Cedar oil, having a similarrefractive index, is often used in this widely adopted practice. Other liquids, including synthetic oils and polymers with refractive indexes close to that of emeralds, such asOpticon, are also used. The least expensive emeralds are often treated with epoxy resins, which are effective for filling stones with many fractures.[14][15] These treatments are typically applied in a vacuum chamber under mild heat, to open the pores of the stone and allow the fracture-filling agent to be absorbed more effectively.[16] The U.S.Federal Trade Commission requires the disclosure of this treatment when an oil-treated emerald is sold.[17] The use of oil is traditional and largely accepted by the gem trade, although oil-treated emeralds are worth much less than untreated emeralds of similar quality. Untreated emeralds must also be accompanied by a certificate from a licensed, independent gemology laboratory. Other treatments, for example the use of green-tinted oil, are not acceptable in the trade.[18] Gems are graded on a four-step scale;none,minor,moderate andhighly enhanced. These categories reflect levels of enhancement, notclarity. A gem gradednone on the enhancement scale may still exhibit visible inclusions. Laboratories apply these criteria differently. Some gemologists consider the mere presence of oil or polymers to constitute enhancement. Others may ignore traces of oil if the presence of the material does not improve the look of the gemstone.[19]
Emeralds in antiquity were mined inAncient Egypt at locations on Mount Smaragdus since 1500 BC, and India and Austria since at least the 14th century AD.[20] The Egyptian mines were exploited on an industrial scale by the Roman and Byzantine Empires, and later by Islamic conquerors. Mining in Egypt ceased with the discovery of the Colombian deposits. Today, only ruins remain in Egypt.[21]
Colombia is by far the world's largest producer of emeralds, constituting 50–95% of the world production, with the number depending on the year, source and grade.[22][23][24][25] Emerald production in Colombia has increased drastically in the last decade, increasing by 78% from 2000 to 2010.[26] The three main emerald mining areas in Colombia areMuzo, Coscuez, andChivor.[27] Rare"trapiche" emeralds are found in Colombia, distinguished by ray-like spokes of dark impurities.
Zambia is the world's second biggest producer, with itsKafubu River area deposits (Kagem Mines) about 45 km (28 mi) southwest of Kitwe responsible for 20% of the world's production of gem-quality stones in 2004.[28] In the first half of 2011, the Kagem Mines produced 3.74 tons of emeralds.[29]
Emeralds are found all over the world in countries such as Afghanistan, Australia, Austria, Brazil,[30] Bulgaria, Cambodia, Canada, China, Egypt, Ethiopia, France, Germany, India, Kazakhstan, Madagascar, Mozambique, Namibia, Nigeria, Norway, Pakistan, Russia, Somalia, South Africa, Spain, Switzerland, Tanzania, the United States, Zambia, and Zimbabwe.[1] In the US, emeralds have been found inConnecticut,Montana,Nevada,North Carolina, andSouth Carolina.[1] In 1998, emeralds were discovered in the Yukon Territory of Canada.[31]
Since the onset of concerns regarding diamond origins, research has been conducted to determine if the mining location could be determined for an emerald already in circulation. Traditional research used qualitative guidelines such as an emerald's color, style and quality of cutting, type of fracture filling, and the anthropological origins of the artifacts bearing the mineral to determine the emerald's mine location. More recent studies usingenergy-dispersive X-ray spectroscopy methods have uncovered trace chemical element differences between emeralds, including ones mined in close proximity to one another. American gemologist David Cronin and his colleagues have extensively examined the chemical signatures of emeralds resulting from fluid dynamics and subtle precipitation mechanisms, and their research demonstrated the chemical homogeneity of emeralds from the same mining location and the statistical differences that exist between emeralds from different mining locations, including those between the three locations: Muzo, Coscuez, and Chivor, in Colombia, South America.[32]
Both hydrothermal andflux-growth synthetics have been produced, and a method has been developed for producing an emerald overgrowth on colorlessberyl. The first commercially successful emerald synthesis process was that ofCarroll Chatham, likely involving a lithium vanadate flux process, as Chatham's emeralds do not have any water and contain traces of vanadate, molybdenum and vanadium.[33] The other large producer of flux emeralds wasPierre Gilson Sr., whose products have been on the market since 1964. Gilson's emeralds are usually grown on natural colorless beryl seeds, which are coated on both sides. Growth occurs at the rate of 1 mm per month, a typical seven-month growth run produces emerald crystals 7 mm thick.[34]
Hydrothermal synthetic emeralds have been attributed toIG Farben, Nacken,Tairus, and others, but the first satisfactory commercial product was that ofJohann Lechleitner ofInnsbruck, Austria, which appeared on the market in the 1960s. These stones were initially sold under the names "Emerita" and "Symeralds", and they were grown as a thin layer of emerald on top of natural colorless beryl stones. Later, from 1965 to 1970, theLinde Division ofUnion Carbide produced completely synthetic emeralds by hydrothermal synthesis. According to their patents (attributable toE.M. Flanigen),[35] acidic conditions are essential to prevent the chromium (which is used as the colorant) from precipitating. Also, it is important that the silicon-containing nutrient be kept away from the other ingredients to prevent nucleation and confine growth to the seed crystals. Growth occurs by a diffusion-reaction process, assisted by convection. The largest producer of hydrothermal emeralds today is Tairus, which has succeeded in synthesizing emeralds with chemical composition similar to emeralds in alkaline deposits in Colombia, and whose products are thus known as “Colombian created emeralds” or “Tairus created emeralds”.[36] Luminescence inultraviolet light is considered a supplementary test when making a natural versus synthetic determination, as many, but not all, natural emeralds are inert to ultraviolet light. Many synthetics are also UV inert.[37]
Emerald made by hydrothermal synthesis
Synthetic emeralds are often referred to as "created", as their chemical and gemological composition is the same as their natural counterparts. The U.S.Federal Trade Commission (FTC) has very strict regulations as to what can and what cannot be called a "synthetic" stone. The FTC says: "§ 23.23(c) It is unfair or deceptive to use the word "laboratory-grown", "laboratory-created", "[manufacturer name]-created", or "synthetic" with the name of any natural stone to describe any industry product unless such industry product has essentially the same optical, physical, and chemical properties as the stone named."[17]
Traditionalalchemical lore ascribes several uses and characteristics to emeralds:
The virtue of the Emerald is to counteract poison. They say that if a venomous animal should look at it, it will become blinded. The gem also acts as a preservative against epilepsy; it cures leprosy, strengthens sight and memory, checks copulation, during which act it will break, if worn at the time on the finger.[39]
According to French writerBrantôme (c. 1540–1614)Hernán Cortés had one of the emeralds which he had looted from Mexicotext engraved,Inter Natos Mulierum non surrexit major ("Among those born of woman there hath not arisen a greater,"Matthew 11:11), in reference toJohn the Baptist. Brantôme considered engraving such a beautiful and simple product of nature sacrilegious and considered this act the cause for Cortez's loss in 1541 of an extremely precious pearl,[note 1] and even for the death of KingCharles IX of France, who died (1574) soon afterward.[40][41]
The chief deity of one of India's most famous temples, theMeenakshi Amman Temple inMadurai, is the goddessMeenakshi, whose idol is traditionally thought to be made of emerald.[42]
Emerald on quartz, from Carnaiba Mine, Pindobaçu, Campo Formoso ultramafic complex, Bahia, Brazil
TheChalk Emerald ring, containing a top-quality 37-carat emerald, in the U.S. National Museum of Natural History
Emerald crystals
A 5-carat emerald from Muzo with hexagonal cross-section
Gachalá Emerald, one of the largest gem emeralds in the world, at 858 carats (171.6 g). Found in 1967 at La Vega de San Juan mine in Gachalá, Colombia. Housed at theNational Museum of Natural History in Washington, D.C.
Rough emerald crystals from Panjshir Valley Afghanistan
Large, di-hexagonal prismatic crystal of 1,390 carats uncut with a deep green color. It is transparent and features few inclusions in the upper 2/3, and is translucent in the lower part. Housed at theMim Museum, Beirut, Lebanon.
^"Romans organized the mines as a multinational business..." Finlay, Victoria. Jewels: A Secret History (Kindle Location 3098). Random House Publishing Group. Kindle Edition.
^Carrillo, V. (2001). Compilación y análisis de la información geológica referente a la explotación esmeraldífera en Colombia. Informe de contrato 124. INGEOMINAS
^O'Donoghue, Michael (1988).Gemstones. Dordrecht: Springer Netherlands. p. 310.ISBN9789400911918.Archived from the original on 30 March 2017.
^Nassau, K. (1980)Gems Made By Man, Gemological Institute of America,ISBN0-87311-016-1.
^Geological Magazine "Hydrothermal process for growing crystals having the structure of beryl in an alkaline halide medium"U.S. patent 3,567,642 Issue date: 2 March 1971
^Ruland, Martin (26 May 2014) [1612]. "Smaragdus".A Lexicon of Alchemy [Lexicon alchemia]. Translated byWaite, Arthur Edward. Altenmünster, Bavaria: Jazzybee Verlag (published 2014).ISBN978-3-8496-4439-0.Archived from the original on 25 June 2022. Retrieved25 June 2022.The virtue of the Emerald is to counteract poison. They say that if a venomous animal should look at it, it will become blinded. The gem also acts as a preservative against epilepsy; it cures leprosy, strengthens sight and memory, checks copulation, during which act it will break, it worn at the time on the finger.
^"Gachala Emerald".National Museum of Natural History. Smithsonian Institution. 2017.Archived from the original on February 11, 2017. RetrievedFebruary 8, 2017.
^Bouillard, J.-C. and Jeanne-Michaud, A. (2016) "101 minéraux et pierres précieuses – qu'il faut avoir vus dans sa vie". Hors collection, Dunod.ISBN2100742272.
Cooper, J. C. (ed.) (1992).Brewer's Myth and Legend. New York: Cassell Publishers Ltd.ISBN0-304-34084-7.
Giuliani, Gaston, Ed. (2022). Émeraudes, tout un monde. Led Editions du Piat,ISBN978-2-917198-51-3
Hurlbut, Cornelius S.; Klein, Cornelis (1985).Manual of Mineralogy (20th ed.). New York: John Wiley and Sons.ISBN0-471-80580-7.
Sinkankas, John (1994).Emerald & Other Beryls. Prescott, Ariz.: Geoscience Press.ISBN0-8019-7114-4.
Tavernier, Jean-Baptiste (1925 [1676]).Travels in India (second edition), Volume II. Edited by William Crooke and translated by V. Ball. London: Oxford University Press.
Weinstein, Michael (1958).The World of Jewel Stones. New York: Sheriden House.OCLC519758.
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