CURRENTLY VIEWING: Iolite
 Iolite (or Cordierite) is a cyclosilicate of magnesium and aluminium. Iron is almost always present and a series exists between Mg-rich cordierite and Fe-rich sekaninaite with a series formula: (Mg,Fe)2Al4Si5O18 to (Fe,Mg)2Al4Si5O18.
Cordierite typically occurs in contact or regional metamorphism of argillaceous rocks. Common associated minerals include: sillimanite, spinel, plagioclase, orthopyroxene, garnet, and anthophyllite. Cordierite also occurs in some granite and pegmatites. Alteration products include mica, chlorite, or talc.
Cordierite ceramic is commonly used in catalytic converters.
Cordierite is named after a French geologist P. L. A. Cordier (1777 - 1861).
As the transparent variety iolite, it is often used as a gemstone. The name iolite comes from the Greek word for violet. Another old name is dichroite a greek word meaning two colored rock a reference to Cordierite's strong pleochroism. Gem quality iolite varies in colour from sapphire blue to blue violet to yellowish gray to light blue as the light angle changes. Gem quality cordierite is found in various places such as Sri Lanka and Burma. Other localities where iolite is found include Australia's Northern Territory, Namibia, Brazil, Tanzania, Madagascar, Connecticut, and the Yellowknife area of the Northwest Territories of Canada. Closely related is Fahlunite, a altered variety of cordierite from the Fahlun Mine, Sweden.
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