A brown, gray, white, or pale green mineral, Al2SiO5, used as a gemstone and for ornamental carvings. Also called fibrolite.
[After Benjamin SILLIMAN.]
Dictionary:
sil·li·ma·nite (sĭl'ə-mə-nīt') ![]() |
A brown, gray, white, or pale green mineral, Al2SiO5, used as a gemstone and for ornamental carvings. Also called fibrolite.
[After Benjamin SILLIMAN.]
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A nesosilicate mineral of composition Al2O[SiO4], crystallizing in the orthorhombic system. Sillimanite commonly occurs in slender crystals or parallel groups, and is frequently fibrous, hence the synonym fibrolite. There is one perfect cleavage, luster is vitreous, color is brown, pale green, or white, hardness is 6–7 on Mohs scale, and the specific gravity is 3.23.
Sillimanite, andalusite, and kyanite are polymorphs of Al2O[SiO4]. The three Al2O[SiO4] polymorphs are important in assessing the metamorphic grade of the rocks in which they crystallized. See also Andalusite; Kyanite; Silicate minerals.
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Environment
Mica schists and gneisses, and in contact metamorphic deposits.
Crystal descriptionUsually in finely fibrous gray or brownish masses, embedded in rock. Very fine needles can form a compact rock (Brazil and New Mexico) that streams wear into interesting shapes (Brazil). Distinct pale blue prismatic crystals, clear and transparent, with good side pinacoidal cleavage in the rare gemmy variety.
Physical propertiesUsually white, sometimes brownish or greenish (gem variety light blue). Luster satiny (glassy when gemmy); hardness 6-7 (but splinters and is difficult to determine; gemmy examples are 7Ɖ); specific gravity 3.2-3.3; fracture splinters lengthwise, but conchoidal breaks across elongation; cleavage perfect pinacoid, but usually fibrous. Translucent to transparent.
CompositionAluminum silicate (63.2% Al 2 O 3 , 36.8% SiO 2 ).
TestsInfusible and insoluble, but the crushed mineral, or a bundle of fibers, turns blue when heated with cobalt nitrate solution (aluminum test).
Distinguishing characteristicsInfusibility distinguishes it from fibrous anthophyllite, which it may resemble (anthophyllite fuses to a black magnetic bead). Hardness and brittleness of the fibers distinguish them from those of asbestos.
OccurrenceRelatively rare, in fibrous, more or less parallel masses in schist, and often altered in part to mica; therefore lacking in normal hardness. Interesting because its Myanmar and Sri Lanka occurrences (where it is found in waterworn, clear, blue, gemmy pebbles) are so unlike the fibrous embedded masses of New England at Worcester, Massachusetts, and Norwich and Willimantic, Connecticut. Also in New York and Pennsylvania. Sometimes, as in North Carolina and Brazil, it is compact enough to form tough waterworn pebbles that may be cut to resemble a cat's-eye. Lately in some abundance in Orissa, India. Pebbles of the compact fibers can water-wear into smooth and shiny surfaces, even more lustrous than waterworn jade masses. Another (historical) name, fibrolite, comes from its appearance; the official name sillimanite was given in honor of Yale's first professor of mineralogy, Benjamin Silliman. New Mexican Indians fashioned many tools from sillimanite masses.
| Wikipedia: Sillimanite |
Sillimanite also called Bucholzite is an alumino-silicate mineral with the chemical formula Al2SiO5. Sillimanite is named after the American chemist Benjamin Silliman (1779-1864).
Contents |
Sillimanite is one of three alumino-silicate polymorphs, the other two being andalusite and kyanite. A common variety of sillimanite is known as fibrolite, so named because the mineral appears like a bunch of fibres twisted together when viewed under thin section or even by the naked eye. Both the fibrous and traditional forms of sillimanite are common in metamorphosed sedimentary rocks. It is an index mineral indicating high-temperature metamorphism.
Sillimanite has been found in Brandywine Springs, New Castle County, Delaware, USA. By suggestion of the members of the Delaware Mineralogical Society, it was named by the State Legislature in 1977 as the Official Mineral of Delaware.
| Crystallographic system | Orthorhombic |
| Colours | White, brown and green |
| Lustre | Silky if in fibrous form, else vitreous |
| Hardness | 7.5 |
| Refractive index | 1.641-1.648 |
| Cleavage | 1 |
| Twinning | n/a |
| Pleochroism | Colourless to pale brown to yellow |
| Type locality | Vltava, Susice, Czech Republic. |
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![]() | 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 | |
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![]() | 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 | |
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