Photo of Sillimanite in Processed & Rough Form
Sillimanite is a mineral with a hardness of 8 out of 10 on the Mohs scale of mineral hardness [?]. These Orthorhombicly structured gems are made of aluminum silicate, their full chemical compound being Al2SiO5.
Sillimanite is a grayish-blue aluminum silicate with an orthorhombic crystal system. It is trimorphic with andalusite and kyanite. All three have the same chemical compound but their atoms each arrange to create three different crystal forms.
It appears as long, slender crystals without distinct terminations, in off-white, gray, brown, pale green, slate-blue, blue-green, and these crystals are often in silky, fibrous aggregates (fibrolite). This fiber sillimanite is mistakenly called "radiated quartz." It also frequently occurs as needle-like crystal inclusions in other minerals, like quartz and feldspars. When it appears as inclusions in rose quartz and other gemstones, it causes that stone to exhibit asterism, star-like rays in reflected light.
It is hard, heavy, with perfect cleavage parallel to its fibers, with uneven fracture. It is transparent to translucent with vitreous to pearly luster. It is insoluble and infusible.
Sillimanite is widespread in high-temperature regional metamorphic rocks and occasionally in pegmatites, where volatile fluid elements in the later stage of magma cooling encourage crystal formation. It also occurs in gneiss, micaschist, granulite, eclogite. Most gem sillimanite is found in gem gravels, carried by fast-flowing water from its headwater rocks to downstream sediment areas.
In the high-elevation Mogok region in Myanmar can be found violet-blue sillimanite stones, and in the Sri Lanka gem gravels, a grey-green chatoyant material is obtained. Group masses of greenish crystals have been found in Bohemia (Czechoslovakia); yellowish crystals in Val di Fassa (Trento, Italy), Bavaria and Saxony (Germany); specimens of chatoyant fibrolite aggregates in Brazil and South Carolina (USA). Blue crystals of sillimanite associated with rubies have been found in sands in Burma and Sri Lanka. Small-sized material similar to the Myanmar specimens is reported from Kenya. Large, remarkably pure masses (85% sillimanite) have been mined in India.
Sillimanite is also called bucholzite fibrolite - very rarely offered as a small gem quality stone but more often as a fibrous aggregate. Greenish or brownish varieties of sillimanite are used as an inferior substitute for jade. This has led to the unfortunate misleading term of 'false jade' to describe what is rightfully sillimanite.
The specific gravity [?] for Sillimanite is 3.25, it's refractive index [?] is 1.66-1.68, and it's double refraction [?] is 0.019.
History
Sillimanite was first described in 1824 after it was found in Connecticut, (USA) and is named after the American chemist Benjamin Silliman, who was one of the first Yale University professors of science and and analyzed many minerals, identifying their constituent elements.
Industrial Usages
Sillimanite is an industrial mineral used in the manufacture of refractories for furnaces, ovens, incinerators, reactors; high-temperature crucibles, and high temperature-resistant ceramics; and glass manufacturing. Chatoyant, green and blue varieties are used in jewelry. Sillimanite is valuable to geological study as a sensitive indicator of the temperature and pressure at which the host rock formed.
It is cut as faceted gemstones and sometimes with blue-green chatoyant effect. Sillimanite is one of the most difficult transparent gem materials to fashion.
You May Also Like...
Petalite: Petalite is a lithium aluminum silicate that is an important ore of lithium. This mineral forms, rarely, as small crystals, which are commonly twinned. More often, petalite forms as large, cleavable masses. It may be white, grey, pinkish, yellow, or colorless. It is transparent to translucent, with a vitreous to pearly luster, and fuses with difficulty. It forms in very coarse-grained, acid igne (read full)
Jadeite: Jadeite is a silicate of sodium and aluminum, and is a member of the Clinopyroxene group of minerals. It is so called because it is the source of one of the ornamental materials commonly known as Jade. It has a monoclinic crystal system, and occurs as granular aggregates of small crystals, but has occasionally been found in crystals of a few centimeters. The color varies a great deal because of t (read full)
Orthoclase: Orthoclase mineral is a silicate of potassium and aluminum, belonging to the Feldspar group. It has the same composition as microcline, but is stable at slightly higher temperatures. It occurs as prismatic, sometimes flat-sided crystals, but in rocks it is usually anhedral. It may be perfectly transparent and yellow or almost colorless, but it is more often semi-opaque and white to grayish-white, (read full)
Kyanite: Kyanite is an aluminum silicate that occurs as elongated and tabular in groups of light-blue crystals darker toward the center, or flat, bladed crystals in schists and gneisses, or as radiating rosettes in quartz. It is trimorphous with sillimanite and andalusite. Kyanite is also known as disthene, meaning, "double strength." This refers to the fact that the hardness along the length of kyanite c (read full)
Euclase: Euclase is a silicate with a monoclinic crystal system. It is considered a very rare gem of light blue color. It appears as long or short prismatic crystals, flattened and transparent. It is colorless, white, green, or blue, commonly a pale aquamarine or green, but crystals of a very fine dark blue (from iron) have been found at the Miami mine in Zimbabwe. Crystals are often striated. It (read full)
