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Chrysoprase – history and present

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The authors present the history of chrysoprase discovery and the progress of knowledge about this material over the millennia, based on the extended review of world literature. Tracing the oldest archaeological artifacts from before 9,000 years, the lens of history turns on a stone that has not been properly identified mineralogically for centuries. In the 1830s, chrysoprase was finally included into the chalcedony group and its green color was associated, very correctly, with nickel compounds dispersed in its structure. After all, the most current mineralogy of chrysoprase is presented on the basis of the results of modern analytical studies. These data clearly indicate that chrysoprase is a mixture of several SiO2 polymorphs with varying degrees of structural order (opal, chalcedony, moganite, quartz). This radically changes the previous taxonomy of chrysoprase and its position in current mineralogical and petrographic systematics.
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1--10
Opis fizyczny
Bibliogr. 72 poz., rys., foto
Twórcy
  • Higher School of Handicraft and Management, 21 Saint Matthias Square, 50-244 Wrocław, Poland
  • Higher School of Handicraft and Management, 21 Saint Matthias Square, 50-244 Wrocław, Poland
  • AGH University of Science and Technology, Department of Mineralogy, Petrography and Geochemistry, Al. Mickiewicza 30, 30-059 Krakow, Poland
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Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c231fe17-e340-4019-87e5-696cecff16ae
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