geodil.jpg

A Geoscience Digital Image Library

678.jpg
TitleOpal and chalcedony
DescriptionThis specimen, 10 cm across, contains both opal and chalcedony. Opal generally shows a “play of colors” called opalescence which gives it rainbow colors – only moderately developed in this specimen. Opal, considered a mineraloid because its structure is not truly crystalline, has chemistry SiO2-nH2O. The amount of water in opal is 5-10% or more. This water can help geologists determine the temperature of the host rock at the time the opal formed. Opal forms in sedimentary environments and as a secondary mineral formed by alteration of high silica igneous extrusive rocks. It's name comes from the Old Indian upala meaning “precious stone.” Chalcedony (white fine-grained material on top of the specimen) is a cyptocrystalline (crystals too small to be seen even by a microscope) variety of quartz.
LocationUSA ▹ Wyoming. Near Yellowstone.
PhotographerShannon Heinle. 2001-06-11.
CollectionUniversity of North Dakota Mineralogy Collection #1572.
Key wordsopal, chalcedony, mineraloid, quartz, cyptocrystalline
Tech details410 KB. Hand specimen. Fujifilm FinePix S1Pro digital camera; 60mm AF Nikon micro lens.
GeoDIL number678