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Encyclopedia > Sillimanite
Sillimanite: Biotite gneiss (Mesozoic and Paleozoic)
Sillimanite: Biotite gneiss (Mesozoic and Paleozoic)

Sillimanite is an alumino-sillicate mineral with the chemical formula Al2SiO5. Sillimanite is named after the American chemist Benjamin Silliman (1779-1824). Sillimanite MzPzbg Biotite gneiss (Mesozoic and Paleozoic): Gray, fine- to coarse-grained, banded biotite gneiss. ... Sillimanite MzPzbg Biotite gneiss (Mesozoic and Paleozoic): Gray, fine- to coarse-grained, banded biotite gneiss. ... This article is about minerals in the geologic sense; for nutrient minerals see dietary mineral; for the band see Mineral (band). ... A chemical formula (also called molecular formula) is a concise way of expressing information about the atoms that constitute a particular chemical compound. ... 1779 was a common year starting on Friday (see link for calendar). ... 1824 was a leap year starting on Thursday (see link for calendar). ...

Contents


Occurrence

Sillimanite is one of three alumino-sillicate 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. In general, a polymorph is something that can exist in several states or forms. ... Andalusite-cordierite schist (Large brown crystals are Andalusite Andalusite is an alumino-silicate mineral with the chemical formula Al2SiO5. ... Kyanite The mineral kyanite is an aluminium silicate of the sillimanite group (along with andalusite and sillimanite), also called alumino-silicate. ... Metamorphism can be defined as the mineralogical, chemical and crystallographic changes in a solid-state rock, i. ... Two types of sedimentary rock: limey shale overlaid by limestone. ...


Details

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.

Rose des Sables (Sand Rose), formed of gypsum crystals In mineralogy and crystallography, a crystal structure is a unique arrangement of atoms in a crystal. ... Mohs scale of mineral hardness characterizes the scratch resistance of various minerals through the ability of a harder material to scratch a softer. ... The parameter used to describe the interaction of electromagnetic radiation with matter is the complex index of refraction, , which is a combination of a real part and an imaginary part. ... Pleochroism is an optical phenomenon where due to double refraction of light by a colored gem or crystal, the light is divided into two paths which are polarized at a 90° angle to each other. ... The Vltava (German: Moldau) is the longest river in the Czech Republic, draining north from its source in Šumava through Český Krumlov, České Budějovice and Prague, merging with the Elbe (Labe) at Mělník. ...

Related minerals

Andalusite-cordierite schist (Large brown crystals are Andalusite Andalusite is an alumino-silicate mineral with the chemical formula Al2SiO5. ... Kyanite The mineral kyanite is an aluminium silicate of the sillimanite group (along with andalusite and sillimanite), also called alumino-silicate. ...

External links


  Results from FactBites:
 
Sillimanite - LoveToKnow 1911 (232 words)
Sillimanite is a characteristic mineral of gneisses and crystalline schists, and it is sometimes a product of contact-metamorphism.
in Bohemia (the Faserkiesel of Lindacker, 1792), with corundum in the Carnatic (fibrolite of comte de Bournon, 1802), Chester in Connecticut (sillimanite of G. Bowen, 1824), Monroe in New York ("monrolite"), Bamle near Brevik in Norway ("bamlite").
Prehistoric implements made of compact sillimanite are found in western Europe, and have a certain resemblance to jade implements.
  More results at FactBites »

 

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