Andalusite

From Wikipedia, the free encyclopedia

Jump to: navigation, search
Andalusite

Dark, rod-like andalusite crystals in a light green cordierite schist matrix (writing pen shows size).
General
Category mineral
Chemical formula Al2SiO5[1]
Identification
Color transparent to opaque brownish or yellowish green to orangy brown;[1] may be pure green,[1] brown,[1] pink,[1] violet (rare),[1] and red
Crystal system orthorhombic[1]
Twinning lamellar
Cleavage distinct in one direction[1]
Fracture uneven to conchoidal[1]
Mohs scale hardness 7 - 7.5[1]
Luster vitreous[1]
Specific gravity 3.17 (+/- .04)
Polish luster vitreous[1]
Optical properties double refractive, biaxial negative; chiastolite has anomalous aggregate reaction.[1] Can also display chatoyancy.
Refractive index 1.634 - 1.643 (+/-.005)[1]
Birefringence .007 - .013[1]
Pleochroism Strong. Brownish to yellowish green and brownish orange to brownish red
Dispersion .016[1]
Ultraviolet fluorescence inert in long wave, inert to moderate green to yellowish green in short wave[1]

Andalusite is an aluminium nesosilicate mineral with the chemical formula Al2SiO5.

The variety chiastolite commonly contains dark inclusions of carbon or clay which form a checker-board pattern when shown in cross-section.

A clear variety first found in Andalusia, Spain can be cut into an interesting gemstone.[2] Faceted andalusite stones give a play of red, green, and yellow colors that resembles a muted form of iridescence, although the colors are actually the result of unusually strong pleochroism.

It is associated with mica schist which increases alkali content in ultimate product and so it has not been exploited economically so far.

Contents

[edit] Occurrence

Andalusite is a common regional metamorphic mineral which forms under low pressure and moderate to high temperatures. Called Lapis Crucifer in ancient texts. The minerals kyanite and sillimanite are polymorphs of andalusite, each occurring under different temperature-pressure regimes and are therefore rarely found together in the same rock. Because of this the three minerals are a useful tool to help identify the pressure-temperature paths of the host rock in which they are found.

It was first reported from Andalucia, Spain in 1789.

[edit] Related minerals

[edit] See also

[edit] References

[edit] Notes