Cordierite
A mineral of the silicate family
Cordierite is a silicate mineral that belongs to the cyclosilicate family. It is known for its distinct pleochroism, which means it can display different colors when viewed from different angles. Cordierite is often used as a gemstone and is sometimes referred to as "iolite" in the gem trade.
Properties
Cordierite is a magnesium iron aluminium cyclosilicate with the chemical formula (Mg,Fe)₂Al₄Si₅O₁₈. It typically forms in metamorphic rocks and is known for its ability to withstand high temperatures, making it useful in various industrial applications.
Physical Characteristics
Cordierite is typically blue to violet in color, although it can also appear in shades of gray, yellow, or green. It has a hardness of 7 to 7.5, making it relatively hard and durable. The mineral has a vitreous to pearly luster and a conchoidal fracture.
Optical Properties
One of the most notable features of cordierite is its strong pleochroism. This optical phenomenon allows the mineral to show different colors when viewed from different angles, typically blue, violet, and yellow-brown. This property is particularly pronounced in gem-quality specimens.
Occurrence
Cordierite is commonly found in metamorphic rocks such as gneiss and schist, where it forms under high-temperature conditions. It can also occur in igneous rocks like granite and pegmatite. Major sources of cordierite include Sri Lanka, India, Madagascar, and the United States.
Uses
Cordierite is primarily used as a gemstone, where it is often marketed under the name "iolite." Its unique pleochroism makes it a popular choice for jewelry. In addition to its use in jewelry, cordierite is also used in industrial applications, particularly in the manufacture of heat-resistant ceramics and catalytic converters.
Gemology
In the gem trade, cordierite is valued for its color and pleochroism. It is often cut into faceted stones to enhance its optical properties. The gemstone is sometimes used as a substitute for sapphire due to its similar appearance.
Pleochroism
Cordierite's pleochroism is a result of its crystal structure, which causes light to be absorbed differently along different crystallographic axes. This property is not only a key identifier for the mineral but also a desirable trait in gemstones.
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