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topaz

  ('păz') pronunciation
n.
    1. A colorless, blue, yellow, brown, or pink aluminum silicate mineral, often found in association with granitic rocks and valued as a gemstone, especially in the brown and pink varieties.
    2. Any of various yellow gemstones, especially a yellow variety of sapphire or corundum.
  1. A light yellow variety of quartz.
  2. Either of two South American hummingbirds (Topaza pyra or T. pella) having colorful plumage.

[Middle English topace, from Old French, from Latin topazus, from Greek topazos.]


 
 

A mineral best known for its use as a gemstone. Crystals are usually colorless but may be red, yellow, green, blue, or brown. The wine-yellow variety is the one usually cut and most highly prized as a gem. Corundum of similar color sometimes goes under the name of Oriental topaz. Citrine, a yellow variety of quartz, is the most common substitute and may be sold as quartz topaz.

Topaz is a nesosilicate with chemical composition Al2SiO4(F,OH)2. The mineral crystallizes in the orthorhombic system and is commonly found in well-developed prismatic crystals with pyramidal terminations. It has a perfect basal cleavage which enables it to be distinguished from minerals otherwise similar in appearance. Hardness is 8 on Mohs scale; specific gravity is 3.4–3.6. See also Hardness scales.

Fine yellow and blue crystals have come from Siberia and much of the wine-yellow gem material from Minas Gerais, Brazil. In the United States topaz has been found near Florissant, Colorado; in Thomas Range, Utah; in San Diego County, California; and near Topsham, Maine. See also Gem; Silicate minerals.


 

Topaz from Minas Gerais state, Brazil
(click to enlarge)
Topaz from Minas Gerais state, Brazil (credit: Lee Boltin)
Aluminum silicate mineral, Al2SiO4(F,OH)2, that is valued as a gemstone. It is formed by fluorine-bearing vapours given off during the last stages of the crystallization of igneous rocks. Pure topaz may be colourless and, when brilliant-cut, has been mistaken for diamond. It may also be various shades of yellow, blue, or brown. Imperial topaz, with vivid reddish orange colour, from Minas Gerais, Braz., is very highly valued.

For more information on topaz, visit Britannica.com.

 
('păz) , aluminum silicate mineral with either hydroxyl radicals or fluorine, Al2SiO4(F,OH)2, used as a gem. It is commonly colorless or some shade of pale yellow to wine-yellow; pale blue and pale green also occur, but natural red stones are uncommon. Some natural yellow stones lose their yellow coloring when heated and become permanently pink (“pinked” topaz). The stone is transparent with a vitreous luster. It has perfect cleavage on the basal pinacoid, but it is nevertheless hard and durable. The brilliant cut is commonly used. Topaz crystals, which are of the orthorhombic system, occur in highly acid igneous rocks, e.g., granites and rhyolites, and in metamorphic rocks, e.g., gneisses and schists. Important sources of topaz are in Russia, Siberia, Brazil, Australia, and Mexico and in New Hampshire, Colorado, and Utah in the United States. The name topaz is commonly but incorrectly used for various other yellow stones, e.g., for citrine quartz.


 

Al
Orthorhombic -- Rhombic bipyramidal

Environment

In pegmatites, seams in granitic rock, high-temperature veins and replacement impregnations, and gas cavities in rhyolite.

Crystal description

Commonly crystallized, often in free-growing transparent crystals, sometimes very large. The c -face, the base, may be conspicuous or may be entirely missing; it is usually present. Also in parallel columnar growths (pycnite); in pseudomorphs after feldspar crystals; and in granular masses. When doubly terminated, "precious" (golden) crystals may appear hemimorphic, for the terminal faces at the two ends of the Brazilian precious topaz are usually unlike.

Physical properties

Colorless, white, pale blue, light yellow, yellow-brown, pinkish brown, pink, and ruby red. Luster glassy; hardness 8; specific gravity 3.5-3.6; fracture conchoidal; cleavage perfect basal. Transparent to translucent.

Composition

Aluminum fluohydroxysilicate (56.5% Al 2 O 3 , 33.3% SiO 2 , and about 10% F and OH). The paragenetical habit differences are great enough to suggest major structural differences, perhaps related to the F and OH content.

Tests

Infusible, and insoluble in all but hydrofluoric acid. The powder turns blue (aluminum test) when moistened with cobalt nitrate and heated.

Distinguishing characteristics

Great hardness and its good cleavage are excellent indications, along with its crystal form and typical occurrence and pegmatitic associations. Beryl fuses on thin edges; quartz decrepitates more violently and easily.

Occurrence

A valuable jewelry stone, especially in the pink, red, and brown hues. Not to be confused with the brown quartz commonly sold in Brazil and other lands (under the name topaz, as in "smoky topaz."

Large topaz crystals are not common in the U.S.; the biggest are probably some crudely shaped white ones found in the pegmatite at Amelia, Virginia, associated with microcline. Clear crystals, to 4-5 in. (10 cm) across and somewhat etched, from Devils Head and Pikes Peak, Colorado; smaller crystals have come from other Colorado localities. Large and deeply etched blue crystals were found at Topsham, Maine, and many 1-2 in. (2-5 cm) crystals were found in small miarolitic cavities in granite with smoky quartz, feldspar, and phenakite at Baldface Mountain, New Hampshire. Less etched, pale blue crystals are found in Mason Co., Texas. Also important in San Diego Co., California, dikes associated with beryl and tourmaline.

Rhyolite extrusions of the Thomas Range, Utah (and, less conspicuously, of Nathrop, Colorado, and New Mexico) contain many gas cavities in which there are 1-in. (3 cm) light brown crystals, which soon fade to colorless on exposure to light. Larger but sandy crystals within the rhyolite, mostly filled with quartz and opaque, are always simpler in their terminations. It is associated in Utah with black bixbyite ([Mn,F] 2 O 3 ) cubes, rosy beryl (not morganite), and in Colorado with spessartine garnet. In San Luis Potosí, Mexico, similar and sometimes larger topaz appears to occur alone or perhaps with cassiterite in the rhyolite seams.

Brazilian topaz is outstanding and comes in pegmatitic colorless and blue crystals, as well as in a series of quartz veins in rich brown gemmy crystals known as "precious topaz." Pink crystals of this type have also been found in nearby hematite mines and lately in Pakistan. Small natural pink Russian topazes from the valley of the Sanarka River resemble some of the brown Brazilian gemstones, with the same crystal habit. Fine blue topaz crystals (and sherry-hued fading to blue) were found years ago in pegmatites in the Ural Mountains; lately large numbers of pale brown crystals, fading to white, have been found in Pakistan.

Though like pegmatite crystals in habit, the small crystals cut for the Saxon crown jewels were straw-hued topazes from veins in and near the "Schneckenstein" (snail stone, from its shape) in the Erzgebirge near the Czechoslovakian border.

Remarks

Golden Brazilian "precious" topaz turns pink on heating, and most pink jewelry topaz has been heated, though recent finds in Pakistan are naturally pink. Topaz is a very attractive and abundant species, characterized by beautiful crystals, placing it among the more popular gemstones with collectors. The common deep blue topaz now so abundant in the jewelry trade is largely irradiated white material; no naturally blue topaz ever reaches such a rich hue.



 
Wikipedia: topaz
Topaz
TopazUSGOV.jpg
an group of topaz crystals on matrix
General
Category Mineral
Chemical formula Al2SiO4(F,OH)2
Identification
Color Clear (if no impurities), blue, brown, orange, gray, yellow, green, pink and reddish pink.
Crystal system orthorhombic
Fracture conchoidal
Mohs Scale hardness 8
Luster Vitreous/glossy
Specific gravity 3.4–3.6

Topaz is a silicate mineral of aluminium and fluorine with the chemical formula Al2SiO4(F,OH)2. It crystallizes in the orthorhombic group and its crystals are mostly prismatic terminated by pyramidal and other faces, the basal pinacoid often being present. It has an easy and perfect basal cleavage, meaning that gemstones or other fine specimens have to be handled with care to avoid developing cleavage flaws. The fracture is conchoidal to uneven. Topaz has a hardness of 8, a specific gravity of 3.4–3.6, and a vitreous luster. Pure topaz is transparent but is usually tinted by impurities; typical topaz is wine or straw-yellow. They may also be white, gray, green, blue, pink or reddish-yellow and transparent or translucent.

Treatments

When heated, yellow topaz often becomes reddish-pink. The color change upon heating was first discovered by a Parisian jeweler around 1750. In particular the yellow Topaz of Brazil has been known to be treated frequently, by wrapping Topaz in Asbestos. Only stones of a brown-yellow color yield the pink; the pale yellow ones usually turn white. The pink color is stable. [1]. Topaz can also be irradiated, turning the stone blue, ranging from a light pure color to very dark almost electric blue. A recent trend in jewelry is the manufacture of topaz specimens that display iridescent colors, by applying a thin layer of titanium oxide via physical vapor deposition, this stone is then sold as 'mystic topaz'.

Localities and occurrence

Topaz is commonly associated with silicic igneous rocks of the granite and rhyolite type. It typically crystallizes in granitic pegmatites or in vapor cavities in rhyolite lava flows like those at Topaz Mountain in western Utah. It may be found with fluorite and cassiterite. It can be found in the Ural and Ilmen mountains, Afghanistan, Czech Republic, Germany, Norway, Pakistan, Italy, Sweden, Japan, Brazil, Mexico, and the United States.

Topaz crystals from Brazilian pegmatites are up to 80 cm x 60 cm x 60 cm in size.[2] The biggest topaz crystal ever found, named "El Dorado", was found in Brazil in 1984. It weighs 6.2 kg and belongs to the British Royal Collection. The famous Braganza diamond is in most likelihood a Topaz. The Topaz of Aurungzebe, observed by Jean Baptiste Tavernier measured 157.75 carats.[3]

Etymology and historical and mythical usage

Colorless topaz, Minas Gerais, Brazil
Enlarge
Colorless topaz, Minas Gerais, Brazil

The name "topaz" is derived from the Greek Τοπάζιος (Τοpáziοs), which was the ancient name of St. John's Island in the Red Sea which was difficult to find and from which a yellow stone (now believed to be chrysolite: yellowish olivine) was mined in ancient times; topaz itself (rather than topazios) wasn't really known about before the classical era. [4] In the Middle Ages the name topaz was used to refer to any yellow gemstone, but now the name is only properly applied to the silicate described above.

Many modern English translations of the Bible, including the King James Version mention topaz in Exodus 28:17 in reference to a stone in the Hoshen: "And thou shalt set in it settings of stones, even four rows of stones: the first row shall be a sardius, a topaz, and a carbuncle: this shall be the first row." However, since these translations as topaz all derive from the Septuagint translation tòpazi[òs], which as mentioned above referred to a yellow stone that wasn't topaz, probably chrysolite, it should be borne in mind that topaz is not meant here. [5] The masoretic text (the Hebrew on which most modern bible translations of the Old Testament are based) has pitdah as the gem the stone is made from; pitdah is of unknown meaning, though scholars think it is related to an Assyrian word meaning flashed. There is a wide range of views among traditional sources about which tribe of the Israelites the stone refers to.

Yellow topaz is the traditional November birthstone (Blue Topaz for December), and the state gemstone for Utah.

References

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  • Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., ISBN 0-471-80580-7
  1. ^ Several Books at the "Pink Topaz" section on Farlang: Fernie: Precious Stones for Curative Wear, London, 1907; Oliver Farrington: Gems and Gem Minerals, Chicago, 1903. Wodiska, A Book of Precious Stones, New York, 1910 (see external links)
  2. ^ The Complete Encyclopedia of Minerals by P. Korbel and M. Novak
  3. ^ Famous and Notheworthy Topazes Rao Bahadur, A Handbook of Precious Stones, Geological Survey of India
  4. ^ Nicols who wrote one of the first systematic treatises on minerals and gemstones dedicated two chapters on the topic in 1652: A Lapidary or History of Gemstones, University of Cambridge, 1652
  5. ^ see for extensive discussion Oliver Farrington, Gems and Gem Minerals, Chicago, 1903. Farrington was curator of Natural History Museum in Chicago.

External links


 
Translations: Translations for: Topaz

Dansk (Danish)
n. - topas

Nederlands (Dutch)
topaas

Français (French)
n. - topaze

Deutsch (German)
n. - Topas

Ελληνική (Greek)
n. - (ορυκτολ.) τοπάζι

Italiano (Italian)
topazio

Português (Portuguese)
n. - topázio (m)

Русский (Russian)
топаз

Español (Spanish)
n. - topacio

Svenska (Swedish)
n. - topas

中文(简体) (Chinese (Simplified))
黄晶, 南美蜂鸟, 黄玉

中文(繁體) (Chinese (Traditional))
n. - 黃晶, 南美蜂鳥, 黃玉

한국어 (Korean)
n. - 황옥, 벌새의 일종

日本語 (Japanese)
n. - 黄玉, トパーズ

العربيه (Arabic)
‏(الاسم) حجر كريم مختلف ألأشكال وألألوان, ألتوباز‏

עברית (Hebrew)
n. - ‮טופז, פטדה‬


 
 

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Copyrights:

Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved.  Read more
Sci-Tech Encyclopedia. McGraw-Hill Encyclopedia of Science and Technology. Copyright © 2005 by The McGraw-Hill Companies, Inc. All rights reserved.  Read more
Britannica Concise Encyclopedia. Britannica Concise Encyclopedia. © 2006 Encyclopædia Britannica, Inc. All rights reserved.  Read more
Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/  Read more
Rock & Mineral Guide. Peterson Field Guide to Rocks and Minerals, by Frederick H. Pough. Copyright © 1998 by Houghton Mifflin Company. Published by Houghton Mifflin Company. All rights reserved.  Read more
Wikipedia. This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Topaz" Read more
Translations. Copyright © 2007, WizCom Technologies Ltd. All rights reserved.  Read more

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