Emerald crystal from Muzo, Colombia
|Crystal system||Hexagonal (6/m 2/m 2/m) Space group: P6/mсc|
|Space group||(6/m 2/m 2/m) – Dihexagonal Dipyramidal|
|Unit cell||a = 9.21 Å, c = 9.19 Å; Z = 2|
|Color||Green shades to colorless|
|Crystal habit||Massive to well Crystalline|
|Cleavage||Imperfect on the |
|Mohs scale hardness||7.5–8|
|Diaphaneity||Transparent to opaque|
|Specific gravity||Average 2.76|
|Optical properties||Uniaxial (-)|
|Refractive index||nω = 1.564–1.595,
nε = 1.568–1.602
|Birefringence||δ = 0.0040–0.0070|
|Ultraviolet fluorescence||None (some fracture filling materials used to improve emerald's clarity do fluoresce, but the stone itself does not)|
Emerald is a gemstone and a variety of the mineral beryl (Be3Al2(SiO3)6) colored green by trace amounts of chromium and sometimes vanadium. Beryl has a hardness of 7.5–8 on the Mohs scale. Most emeralds are highly included, so their toughness (resistance to breakage) is classified as generally poor. Emerald is a cyclosilicate.
The word "emerald" is derived (via Old French: esmeraude and Middle English: emeraude), from Vulgar Latin: esmaralda/esmaraldus, a variant of Latin smaragdus, which originated in Ancient Greek: σμάραγδος (smaragdos; "green gem").
Emeralds, like all colored gemstones, are graded using four basic parameters–the four Cs of Connoisseurship: Color, Clarity, Cut and Carat weight. Before the 20th century, jewelers used the term water, as in "a gem of the finest water", to express the combination of two qualities: color and clarity. Normally, in the grading of 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 green hue as described below, but also a high degree of transparency to be considered a top gem.
In the 1960s, the American jewelry industry changed the definition of "emerald" to include the green vanadium-bearing beryl as emerald. As a result, vanadium emeralds purchased as emeralds in the United States are not recognized as such in the UK 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".
In gemology, color is divided into three components: hue, saturation, and tone. 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 emerald; light-toned gems are known instead by the species name green beryl. The finest emerald are approximately 75% tone on a scale where 0% tone would be colorless and 100% would be opaque black. In addition, a fine emerald should be well saturated and have a hue that is bright (vivid). Gray is the normal saturation modifier or mask found in emerald; a grayish-green hue is a dull-green hue.
Emerald tends to have numerous inclusions and surface breaking fissures. Unlike diamond, where the loupe standard, i.e. 10× magnification, is used to grade clarity, emerald is graded by eye. Thus, if an emerald has no visible inclusions 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 sometime described as "jardin" (French for 'garden'), because of their mossy appearance. 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. The relative non-uniformity motivates the cutting of emeralds in cabochon 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 similar refractive index, is often used in this widely adopted practice. Other liquids, including synthetic oils and polymers with refractive indexes close to that of emerald, such as Opticon, are also used. 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. The U.S. Federal Trade Commission requires the disclosure of this treatment when an oil treated emerald is sold. The use of oil is traditional and largely accepted by the gem trade, although oil treated emeralds are worth much less than un-treated emeralds of similar quality. Other treatments, for example the use of green-tinted oil, are not acceptable in the trade. Gems are graded on a four-step scale; none, minor, moderate and highly enhanced. These categories reflect levels of enhancement, not clarity. A gem graded none 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.
Emeralds in antiquity have been mined in Egypt since 1500 BCE, and India, and Austria since at least the 14th century CE.
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. Emerald production in Colombia has increased drastically in the last decade, increasing by 78% from 2000 to 2010. The three main emerald mining areas in Colombia are Muzo, Coscuez, and Chivor. Rare "trapiche" emeralds are found in Colombia, distinguished by ray-like spokes of dark impurities.
Zambia is the world's second biggest producer, with its Kafubu 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. In the first half of 2011 the Kagem mines produced 3.74 tons of emeralds.
Emeralds are found all over the world in countries such as Afghanistan, Australia, Austria, Brazil, Bulgaria, Cambodia, Canada, China, Egypt, Ethiopia, France, Germany, India, Italy, Kazakhstan, Madagascar, Mozambique, Namibia, Nigeria, Norway, Pakistan, Russia, Somalia, South Africa, Spain, Switzerland, Tanzania, the United States, Zambia, and Zimbabwe. In the US, emeralds have been found in Connecticut, Montana, Nevada, North Carolina, and South Carolina. In Canada, in 1997 emeralds were discovered in the Yukon.
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/or the anthropological origins of the artifacts bearing the mineral to determine the emerald's mine location. More recent studies using energy dispersive X-ray spectroscopy methods have uncovered trace chemical element differences between emeralds; even emeralds mined within 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.
Both hydrothermal and flux-growth synthetics have been produced, and a method has been developed for producing an emerald overgrowth on colorless beryl. The first commercially successful emerald synthesis process was that of Carroll 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. The other large producer of flux emeralds was Pierre 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 producing emerald crystals of 7 mm of thickness. Gilson sold his production laboratory to a Japanese firm in the 1980s, but production has since ceased; so has Chatham's, after the 1989 San Francisco earthquake.
Hydrothermal synthetic emeralds have been attributed to IG Farben, Nacken, Tairus, and others, but the first satisfactory commercial product was that of Johann Lechleitner of Innsbruck, 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. Although not much is known about the original process, it is assumed that Leichleitner emeralds were grown in acid conditions. Later, from 1965 to 1970, the Linde Division of Union Carbide produced completely synthetic emeralds by hydrothermal synthesis. According to their patents (attributable to E.M. Flanigen), 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 in Russia, 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”. Luminescence in ultraviolet light is considered a supplementary test when making a natural vs. synthetic determination, as many, but not all, natural emeralds are inert to ultraviolet light. Many synthetics are also UV inert.
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 "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."
Emerald is regarded as the traditional birthstone for May as well as the traditional gemstone for the astrological signs of Taurus, Gemini, and sometimes Cancer.
One of the quainter anecdotes about emeralds was told by the 16th-century historian Brantôme, who referred to the many impressive emeralds the Spanish under Cortez had brought back to Europe from Latin America. On one of Cortez's most notable emeralds he had the text engraved, Inter Natos Mulierum non sur-rexit mayor ("Among those born of woman there hath not arisen a greater," Matthew 11:11) which referred to John the Baptist. Brantôme considered engraving such a beautiful and simple product of nature sacrilegious and considered this act the cause for Cortez's loss of an extremely precious pearl (to which he dedicated a work, A beautiful and incomparable pearl), and even for the death of King Charles IX of France, who died soon afterward.
The chief deity of one of India's most famous temple, the Meenakshi Amman Temple in Madurai, is the goddess Meenakshi, whose idol is traditionally thought to be made of emerald.
|Bahia Emerald||Brazil, 2001||180,000 carats, crystals in host rock|
|Carolina Emperor||United States, 2009||310 carats uncut, 64.8 carats cut||North Carolina Museum of Natural Sciences, Raleigh|
|Chalk Emerald||Colombia||38.40 carats cut, then recut to 37.82 carats||National Museum of Natural History, Washington|
|Duke of Devonshire Emerald||Colombia, before 1831||1,383.93 carats uncut||Natural History Museum, London|
|Emerald of Saint Louis||Austria, probably Habachtal||51.60 carats cut||National Museum of Natural History, Paris|
|Gachalá Emerald||Colombia, 1967||858 carats uncut||National Museum of Natural History, Washington|
|Mogul Mughal Emerald||Colombia, 1107 A.H. (1695-1696 AD)||217.80 carats cut||Museum of Islamic Art, Doha, Qatar|
|Patricia Emerald||Colombia, 1920||632 carats uncut, dihexagonal (12 sided)||American Museum of Natural History, New York|
The Chalk Emerald ring, containing a top-quality 37-carat emerald, in the U.S. National Museum of Natural History
Emerald crystal (about 1 cm) in calcite matrix, Muzo, Colombia
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 the National Museum of Natural History in Washington, D.C.
|Wikimedia Commons has media related to Emeralds.|
|Main mining areas||
|Individual emeralds (ct)||
العربية زمرد ▪ Aragonés Esmeralda ▪ Asturianu Esmeralda ▪ Azərbaycanca Zümrüd ▪ বাংলা পান্না ▪ Башҡортса Зөбәржәт ▪ Беларуская Ізумруд ▪ Беларуская (тарашкевіца) Смарагд ▪ Български Смарагд ▪ Boarisch Smarogt ▪ Bosanski Smaragd ▪ Brezhoneg Emrodez ▪ Català Maragda ▪ Čeština Smaragd ▪ Dansk Smaragd ▪ Deutsch Smaragd ▪ Eesti Smaragd ▪ Ελληνικά Σμαράγδι ▪ Español Esmeralda ▪ Esperanto Smeraldo ▪ Euskara Esmeralda ▪ فارسی زمرد ▪ Français Émeraude ▪ Gaeilge Smaragaid ▪ Galego Esmeralda ▪ 한국어 에메랄드 ▪ Հայերեն Զմրուխտ ▪ हिन्दी पन्ना ▪ Hrvatski Smaragd ▪ Ido Smeraldo ▪ বিষ্ণুপ্রিয়া মণিপুরী এসমেরআলডা ▪ Bahasa Indonesia Zamrud ▪ Íslenska Smaragður ▪ Italiano Smeraldo ▪ עברית ברקת ▪ Basa Jawa Zamrud ▪ ಕನ್ನಡ ಪಚ್ಚೆ ▪ ქართული ზურმუხტი ▪ Kaszëbsczi Szmaragd ▪ Қазақша Замартас ▪ Kiswahili Zumaridi ▪ Latina Smaragdus ▪ Latviešu Smaragds ▪ Lietuvių Smaragdas ▪ Magyar Smaragd ▪ Македонски Смарагд ▪ മലയാളം മരതകം ▪ مصرى زمرد ▪ Bahasa Melayu Zamrud ▪ Nāhuatl Quetzalitztli ▪ Nederlands Smaragd ▪ 日本語 エメラルド ▪ Norsk bokmål Smaragd ▪ Norsk nynorsk Smaragd ▪ Олык марий Изумруд ▪ Oʻzbekcha/ўзбекча Zumrad ▪ پنجابی زمرد ▪ پښتو زمرد ▪ Polski Szmaragd ▪ Português Esmeralda ▪ Română Smarald ▪ Runa Simi Q'umir umiña ▪ Русский Изумруд ▪ Scots Emerant ▪ Simple English Emerald ▪ سنڌي زمرد ▪ Slovenčina Smaragd ▪ Slovenščina Smaragd ▪ Српски / srpski Смарагд ▪ Srpskohrvatski / српскохрватски Smaragd ▪ Suomi Smaragdi ▪ Svenska Smaragd ▪ தமிழ் மரகதம் ▪ తెలుగు మరకతము ▪ ไทย มรกต ▪ Тоҷикӣ Зумуррад ▪ Türkçe Zümrüt ▪ Українська Смарагд ▪ اردو زمرد ▪ ئۇيغۇرچە / Uyghurche ياقۇت رەڭلىك ▪ Tiếng Việt Ngọc lục bảo ▪ 粵語 呂宋綠 ▪ 中文 祖母綠 ▪