tourmaline

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tourmaline

(to͝or`məlĭn, –lēn), complex borosilicate mineral with varying amounts of aluminum, iron, magnesium, sodium, lithium, potassium, and sometimes other elements, used as a gem. It occurs in prismatic crystals, commonly three-sided, six-sided, or nine-sided, and striated vertically. Different crystal forms are usually present at opposite ends of the vertical axis. The luster is vitreous. Colors are red and pink (rubellite), blue (indicolite, or Brazilian sapphire), green (Brazilian emerald), yellow, violet-red, and black (schorl). Colorless varieties are called achroite. Two or more colors may occur in the same stone, the colors being arranged in zones or bands with sharp boundaries between them. Some Brazilian stones have a red core with a green exterior, separated by a colorless band; some stones from California are green within and red outside. The variations in color are, of course, dependent on the variations in chemical composition. Tourmalines are found in pegmatite veins in granites, gneisses, schists, and crystalline limestone. Sources of the gem include Elba, Madagascar, Myanmar, Sri Lanka, the Urals, Siberia, Brazil, and Maine, Connecticut, and California in the United States.

Tourmaline

 

a boron-containing aluminosilicate mineral of complex, variable composition; a member of the cyclosilicate class of silicates with the general formula

AB3C6(Si6O18)(BO3)3(OH, F, O)4

where A = Na, Ca; B = Mg, Fe2+, Fe3+, Li, Mn, Al; and C = Al, Fe3+. The highly complex tourmaline structure is based on the six-member rings of silicon-oxygen tetrahedrons (Si6O18), which are joined together by BO3 triangles.

Variations in the composition of the B and C cations give rise to different varieties of tourmaline. Examples include the iron-rich varieties schorl (black), verdelite (green), and indicolite (dark blue), the magnesium-rich variety dravite (brownish yellow), the lithium varieties elbaite (lilac pink) and rubellite (dark pink), and the manganese variety tsilaisite. Bright green chromium-bearing varieties of tourmaline are also known. Some tourmaline crystals exhibit pleochroism. Tourmaline crystallizes in the trigonal system to form prismatic crystals having a triangular cross section and characteristic vertical striations. Columnar masses (tourmaline “suns”) are also common.

Tourmaline has a hardness of 7–7.5 on Mohs’ scale and a density of 3,000–3,200 kg/m3. Because the mineral is piezoelectric, large iron-free crystals are used as hydrostatic pressure gauges; the crystals also find use in acoustics, optics, and radio engineering. The double refraction exhibited by tourmaline is used in tourmaline wedges, devices for demonstrating the polarization of light.

Tourmaline is a widespread endogenic high-temperature mineral; it is encountered in metasomatically transformed granites, mica schists, phyllites, and gneisses. The mineral is common in granitic pegmatites, hydrothermal deposits (copper-tourmaline), and greisens. It resists weathering and occurs in placer deposits.

Beautifully colored, transparent varieties of tourmaline (rubellite, bluish green Brazilian sapphire) are precious stones of order II. Deposits of precious varieties are found in the USSR (Urals, Transbaikalia), Brazil (Minas Gerais), Madagascar, and Sri Lanka. Tourmaline is obtained in the laboratory through hydrothermal synthesis.

L. V. BERSHOV

tourmaline

[′tu̇r·mə‚lēn]
(mineralogy)
(Na,Ca)(Al,Fe,Li,Mg)3 Al6(BO3)3Si6O18(OH)4 Any of a group of cyclosilicate minerals with a complex chemical composition, vitreous to resinous luster, and variable color; crystallizes in the ditrigonal-pyramidal class of the hexagonal system, has piezoelectric properties, and is used as a gemstone.

tourmaline

October alternate birthstone. [Am. Gem Symbolism: Kunz, 320]

tourmaline

any of a group of hard glassy minerals of variable colour consisting of complex borosilicates of aluminium with quantities of lithium, sodium, calcium, potassium, iron, and magnesium in hexagonal crystalline form: used in optical and electrical equipment and in jewellery
References in periodicals archive ?
From the big pocket we drove 120 feet northwest, following some very good signs, but netted only a meager little pocket of small blue indicolite tourmalines. Extending the tunnel another 90 feet northwest turned up nothing.
Howie, "Lithium tourmalines from the Meldon aplite, Devonshire, England," Mineralogical Magazine, vol.
Refraction anomalies in tourmalines. Journal of Gemmology, 10(6), 194, http://dx.doi.org/10.15506/ jog.1967.10.6.194.
In the past few years, though, copper-bearing tourmaline from Nigeria and Mozambique has come onto the market.
Tourmaline, with the chemical formula of Na[R.sub.3][Al.sub.6](-[Si.sub.6][O.sub.18]) [(B[O.sub.3]).sub.3] [(OH,F).sub.4] (R is Mg, Fe, Li, or Mn) [3-5], is a natural cyclosilicate mineral.
In the past few years, a relatively new alluvial deposit of tourmaline was found at Maraca, Mozambique.
I assumed that this was the source for the very alluvially rounded tourmalines that I had seen in the market in Luc Yen.
The Minh Tien pegmatite, located a few kilometers southeast of the town of Luc Yen in northern Vietnam, has yielded large and attractive divergent clusters of pink and raspberry-red to yellow-green and yellow-orange tourmaline (elbaite, rossmanite and possibly liddicoatite) in recent years.
Roy Duran, Finer Jewelry Inc., Chicago, Illinois, USA, for assorted orange and colour-change sapphires; small Colombian emerald crystals; a carved amethyst; a jadeite bead; cabochons of synthetic ruby, tourmaline and 'white garnet'; and faceted aquamarine, garnet, peridot and sapphire.
His first ad in The Oregon Mineralogist in December 1933 offered a stock of several thousand terminated California tourmaline crystals.
* 'The Color Palette of the Tourmalines' illustrates the tremendous variety of colours seen in faceted gemstones and in crystals.
Thanks to countless borings and tunnelings, this hill had long since become famous in mineral-collecting circles: many of the best tourmalines in existence had come from here!