Amethyst
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Amethyst is a violet variety of quartz. The name comes from the Koine Greek {{#invoke:Lang|lang}} {{#invoke:Lang|lang}} from {{#invoke:Lang|lang}}- {{#invoke:Lang|lang}}, "not" and {{#invoke:Lang|lang}} (Ancient Greek) Template:Transliteration / {{#invoke:Lang|lang}} Template:Transliteration (Modern Greek), "intoxicate", a reference to the belief that the stone protected its owner from drunkenness.<ref name=EB1911>{{#if: |
|{{#ifeq: Amethyst | |{{#ifeq: | |public domain: }}{{#invoke:template wrapper|{{#if:|list|wrap}}|_template=cite EB1911 |_exclude=footnote, inline, noicon, no-icon, noprescript, no-prescript, _debug| }} | }} }}{{#ifeq: | |{{#ifeq: y | |This article |One or more of the preceding sentences }} incorporates text from a publication now in the
| noicon=1 }}{{#ifeq: ||}}</ref> Ancient Greeks wore amethyst and carved drinking vessels from it in the belief that it would prevent intoxication.
Amethyst, a semiprecious stone, is often used in jewelry.
StructureEdit
Amethyst is a violet variety of quartz (Template:Chem) and owes its violet color to irradiation, impurities of iron (Template:Chem) and in some cases other transition metals, and the presence of other trace elements, which result in complex crystal lattice substitutions.<ref> Template:Cite book </ref><ref name="scielo.br"> Template:Cite journal </ref><ref name=ODongh-2006> Template:Cite book </ref> The irradiation causes the iron Template:Chem ions that replace Si in the lattice to lose an electron and form a Template:Chem0 color center.<ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref> 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 toneEdit
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.<ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref> 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.<ref name=WiseSecrets1> Template:Cite book </ref> "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.<ref> {{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Green quartz is sometimes called green amethyst; the scientific name is prasiolite.<ref name=Gemdat> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref> 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.<ref> Template:Cite journal </ref><ref> Template:Cite journal </ref>Template:Multiple image
The color of amethyst has been demonstrated to result from substitution by irradiation of trivalent iron (Fe3+) for silicon in the structure,<ref name=ODongh-2006/><ref> Template:Cite book </ref> in the presence of trace elements of large ionic radius,<ref name="scielo.br"/> 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,<ref name=ODongh-2006/> but when heated, turns yellow-orange, yellow-brown, or dark brownish and may resemble citrine,<ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref> 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.<ref name=ODongh-2006/> It does not fluoresce under either short-wave or long-wave UV light.
Geographic distributionEdit
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.<ref name=amethnyst-2000> Template:Cite journal </ref>
Amethyst is produced in abundance in the state of Rio Grande do Sul in Brazil where it occurs in large geodes within volcanic rocks.<ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref><ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref><ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref><ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref> 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.<ref name="amethnyst-2000"/>
Amethyst is also found and mined in South Korea.<ref> Template:Cite journal </ref> The large opencast amethyst vein at Maissau, Lower Austria, was historically important,<ref name="EB1911" /> but is no longer included among significant producers.<ref name="amethnyst-2000" /> Much fine amethyst comes from Russia, especially near Mursinka in the Ekaterinburg district, where it occurs in drusy cavities in granitic rocks.<ref name="EB1911" /><ref name="amethnyst-2000" /> Amethyst was historically mined in many localities in south India,<ref name="EB1911" /> though these are no longer significant producers.<ref name="amethnyst-2000" /> One of the largest global amethyst producers is Zambia in southern Africa, with an annual production around 1000 tons.<ref> Template:Cite journal </ref>
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.<ref name="amethnyst-2000"/>
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.<ref name=EB1911/>
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.<ref name=amethnyst-2000/>
Amethyst is the official state gemstone of South Carolina. Several South Carolina amethysts are on display at the Smithsonian Museum of Natural History.<ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref>
HistoryEdit
Amethyst was used as a gemstone by the ancient Egyptians and was largely employed in antiquity for intaglio engraved gems.<ref name=castellani> Template:Cite book — Castellani was a 19th century Italian jeweler, now famous </ref>
The ancient Greeks believed amethyst gems could prevent intoxication,<ref name=smith> Template:Cite book </ref> while medieval European soldiers wore amethyst amulets as protection in battle in the belief that amethysts heal people and keep them cool-headed.<ref name=Kunz-1913> Template:Cite book </ref>Template:Rp Beads of amethyst were found in Anglo-Saxon graves in England.<ref> Template:Cite book </ref> 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.<ref> Template:Cite book name=google </ref>
A large geode, or "amethyst-grotto", from near Santa Cruz in southern Brazil was presented at a 1902 exhibition in Düsseldorf, Germany.<ref name=EB1911/>
Synthetic amethystEdit
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<ref>{{#invoke:citation/CS1|citation |CitationClass=web }} </ref>) 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.<ref name="WiseSecrets1"/>
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".<ref name=EB1911/><ref> Template:Cite book </ref>
Cultural historyEdit
Ancient GreeceEdit
The Greek word {{#invoke:Lang|lang}} may be translated as "not drunken", from Greek {{#invoke:Lang|lang}}, "not" + Template:Transliteration, "intoxicated". Amethyst was considered to be a strong antidote against drunkenness.Template: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.Template:Efn<ref name=Kunz-1913/>Template:Rp
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.<ref> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref>
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.<ref>Nonnus, Dionysiaca, 12. 380</ref>
Other cultural associationsEdit
Tibetans consider amethyst sacred to the Buddha and make prayer beads from it.<ref> Template:Cite book </ref>Template:Full citation Amethyst is considered the birthstone of February.<ref name=americangemsociety> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref> In the Middle Ages, it was considered a symbol of royalty and used to decorate English regalia.<ref name=americangemsociety/> 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.<ref name="Geary-Whelen-2008"> Template:Cite book </ref>
ValueEdit
Template:Multiple image 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.<ref name=Geary-Whelen-2008/> It is now considered a semiprecious stone.<ref> Template:Cite journal </ref>
Collectors look for depth of color, possibly with red flashes if cut conventionally.<ref name=CIBJO> Template:Cite book </ref> 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.<ref name=gemsociety> {{#invoke:citation/CS1|citation |CitationClass=web }} </ref>
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.<ref name=WiseSecrets1/>
Handling and careEdit
The most suitable setting for gem amethyst is a prong or a bezel setting. The channel method must be used with caution.<ref name=GIA-GemDurDes> Template:Cite report </ref>
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.<ref name=GIA-GemDurDes/>
FootnotesEdit
See alsoEdit
ReferencesEdit
External linksEdit
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