Fluorescent minerals

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Fluorescent minerals

Description

Minerals that have the unique physical property to absorb light and one wavelength and instantaneously release it at a different wavelength, resulting in a temporary color change to the eye of the human observer. Only about 15% of minerals are able to fluoresce. The fluorescence is usually due to a cation activator, such as: tungsten, molybdenum, lead, boron, titanium, manganese, uranium, and chromium, but some rare earth elements are also able to contribute to the phenomenon. Some trace elements, such as iron or copper, can quench the fluorscence. Most minerals fluoresce a single color, but some may have multiple colors; for example calcite can fluoresce red, blue, white, pink, green and orange. Because of the potential for many varying factors, the fluorescence of mineral is not typically used for its identification.

Other Properties

Mineral Composition Visible color Fluorescent color
Apatite Ca5(PO4)3(F,Cl,OH) pale green to purple pink, blue, greenish yellow
Calcite CaCO3 colorless to white red, blue, pink, green, orange
Cerrusite PbCO3 colorless to white yellowish
Chalcedony SiO2 white, blue, pink variable
Corundum Al2O3 red (ruby), blue (sapphire) red (ruby), none (sapphire)
Fluorite CaF2 colorless to white blue-violet
Quartz SiO2 colorless, purple variable
Rhyolite PbCO3 colorless to white yellowish
Sphalerite (Zn,Fe)S yellow, brown, gray, black lighter specimens = yellowish
Willemite Zn2SiO4 colorless, white, gray, red, brown strong white

Raman

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Additional Information

J. Ogden, Jewelry of the Ancient World, Rizzoli International Publications, New York, 1982.

Comparisons

Properties of Common Abrasives

Properties of Common Gemstones

Natural and Simulated Diamonds

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