Cordierite is a mineral with a pronounced property of dichroism, which was discovered during its study. Dichroism is the property of absorbing light differently depending on its polarization. It is typical for contact-metamorphic rocks in conditions of high content of aluminum and magnesium. Cordierite easily changes, turning into muscovite and chlorite. Quality cordierite is used by jewelers as a precious stone.
You can see cordierite stone for sale and buy it in the Minerals of Russia online store.
General | |
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Category | Cyclosilicate |
Formula (repeating unit) |
(Mg,Fe)2Al4Si5O18 |
IMA symbol | Crd |
Strunz classification | 9.CJ.10 |
Dana classification | 61.02.01.01 Cordierite group |
Crystal system | Orthorhombic |
Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Cccm |
Unit cell | a = 17.079 Å, b = 9.730 Å, c = 9.356 Å; Z = 4 |
Identification | |
Color | Blue, smoky blue, bluish violet; greenish, yellowish brown, gray; colorless to very pale blue in thin section in transmitted light |
Crystal habit | Pseudo-hexagonal prismatic twins, as imbedded grains, and massive |
Twinning | Common on {110}, {130}, simple, lamellar, cyclical |
Cleavage | Fair on {100}, poor on {001} and {010} |
Fracture | Subconchoidal |
Tenacity | Brittle |
Mohs scale hardness | 7 - 7.5 |
Luster | Greasy or vitreous |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.57 - 2.66 |
Optical properties | Usually optically (-), sometimes (+); 2V = 0-90° |
Refractive index | nα = 1.527 - 1.560 nβ = 1.532 - 1.574 nγ = 1.538 - 1.578 Indices increase with Fe content. |
Pleochroism | X = pale yellow, green; Y = violet, blue-violet; Z = pale blue |
Fusibility | on thin edges |
Diagnostic features | Resembles quartz, can be distinguished by pleochroism. Can be distinguished from corundum by its lower hardness |