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A Geoscience Digital Image Library

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TitleFire opal
DescriptionOpal (rainbow colored) is considered a mineraloid because its structure is not truly crystalline. The most striking quality of opal is its ability to refract and reflect specific wavelengths of light (its “opalescence”) which gives it a play of colors. Opal's chemistry is SiO2-nH2O. The amount of water is generally 5-10% or more. The amount of water depends on the temperature of the host rock at the time the opal formed. Opal forms in sedimentary environments, and as a secondary mineral in high-silica extrusive rocks. It's name comes from the Old Indian upala meaning “precious stone.” This sample is 6 cm across.
LocationUSA ▹ Idaho
PhotographerShannon Heinle. 2001-06-18.
CollectionUniversity of North Dakota Mineralogy Collection #1626.
Key wordsopal, mineraloid
Tech details425 KB. Hand specimen. Fujifilm FinePix S1Pro digital camera; 60mm AF Nikon micro lens.
GeoDIL number780