| Title | Opal and chalcedony | 
| Description | This 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. | 
| Location | USA ▹ Wyoming. Near Yellowstone. | 
| Photographer | Shannon Heinle. 2001-06-11. | 
| Collection | University of North Dakota Mineralogy Collection #1572. | 
| Key words | opal, chalcedony, mineraloid, quartz, cyptocrystalline | 
| Tech details | 410 KB. Hand specimen. Fujifilm FinePix S1Pro digital camera; 60mm AF Nikon micro lens. | 
| GeoDIL number | 678 | 
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