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Timestamp: 2019-04-20 10:56:19+00:00

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Smoky Quartz: Mineral information, data and localities.
A smoky-gray, brown to black variety of quartz that owes its color to gamma irradiation and the presence of traces of aluminum built into its crystal lattice (Griffiths et al, 1954; O'Brien, 1955). The irradiation causes the aluminum Al(+3) atoms that replace Si(+4) in the lattice in a [AlO4]- group to transfer an electron to a neighboring monovalent cation (often Li+) and form a [AlO4/Metal0]0 color center (O'Brien, 1955).
The name Morion is used for black smoky quartz.
Smoky quartz is dichroic (from darker yellow-brown to lighter red-brown) when viewed in polarized light. The photo to the left shows the change of color in a smoky quartz crystal that is rotated in front of an LCD display that serves as a source of polarized light.
The color of smoky quartz is sensitive to heat and will pale at temperatures above 200-300°C or by prolonged exposure to UV light. This loss of color can be reverted by gamma irradiation of the crystals.
Smoky quartz can be found in many different environments but is most characteristic for pockets in igneous rocks and pegmatites. The quartz grains in granites and related rocks are often smoky.
Smoky quartz shows many different habits and crystallographic forms, but needle-like crystals of smoky color are not known.
Crystals that grew at relatively high temperatures, in particular macromosaic quartz crystals like those found in pegmatites and alpine-type fissures are often evenly colored, whereas crystals from other environments often show a color zonation in the form of multiple phantoms. In scepters and skeleton quartz, the color may be more intense along the edges of the crystal.
Note: Very often black or brown crystals that are colored by inclusions of minerals or organic matter are erroneously called "smoky quartz" or "morion". Typical examples of such misnomers are black quartz crystals embedded in sedimentary rocks, like those found in gypsum, anhydrite, and limestone in Italy and Spain. True smoky quartz can be distinguished from crystals that are colored by inclusions by its dichroism.
Visit gemdat.org for gemological information about Smoky Quartz.
Microcline 663 photos of Smoky Quartz associated with Microcline on mindat.org.
Spessartine 654 photos of Smoky Quartz associated with Spessartine on mindat.org.
Amethyst 556 photos of Smoky Quartz associated with Amethyst on mindat.org.
Albite 520 photos of Smoky Quartz associated with Albite on mindat.org.
Fluorite 318 photos of Smoky Quartz associated with Fluorite on mindat.org.
Muscovite 307 photos of Smoky Quartz associated with Muscovite on mindat.org.
Schorl 265 photos of Smoky Quartz associated with Schorl on mindat.org.
Amazonite 252 photos of Smoky Quartz associated with Amazonite on mindat.org.
Hematite 250 photos of Smoky Quartz associated with Hematite on mindat.org.
Orthoclase 233 photos of Smoky Quartz associated with Orthoclase on mindat.org.
Quartz is usually quite harmless unless broken or powdered. Broken crystals and masses may have razor-sharp edges that can easily cut skin and flesh. Handle with care. Do not grind dry since long-term exposure to finely ground powder may lead to silicosis.
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The following Smoky Quartz specimens are currently listed for sale on minfind.com.
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Verbal communication 2.8.2016 by Väinö Kotilainen, who helped prof Martti Lehtinen to move the big crystals to museum.
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Hartmut Hensel collection, Neustadt a. d. Wstr.
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Pezzotta, Federico and Guastoni, Alessandro, The New Discovery of a LCT Pegmatite in the Adamello Massif, Central Southern Alps, Italy; Museo Civico di Storia Naturale, Milan, Italy.; Diella, V., Pezzotta, F., Bocchio, R., Marinoni, N., Cámara, F., Langone, A., Adamo, I., Lanzafame, G. (2018): Gem-quality tourmaline from LCT pegmatite in Adamello Massif, Central Southern Alps, Italy: An investigation of its mineralogy, crystallography and 3D inclusions. Minerals 8, 593.
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widespread in numerous collections; Yamada, S. (2004) Nihonsan-koubutsu Gojuon-hairetsu Sanchi-ichiranhyou (111 pp.); ex-Okamoto collection, now (2015) on display at Hakusekikan museum, Hirukawa.
Alfredo Petrov specimens, received from Colorstone Mithrill, Tokyo.
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Wolfgang Hampel, site visit August 2005.
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Geological Survey of Norway. The Industrial Mineral Database. Deposit Area 928 - 337. Orremyråsen (Updated 27. Apr. 2007).
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Jan Roger Moe collection; Larsen, K. E. (2015). Noen funn av mineraler i Norge 2013-2015. Norsk Mineralsymposium 2015, 79-88.
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Anonymous: (1983): Jensen-skjerpene ( P4-16). DG-nytt [A local magazine for the Drammen geological society, Norway] nr 5, 1983, p.14.
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Anonymous: (1983): Hørtekollen flusspatgruve (D5-01). DG-nytt [A local magazine for the Drammen geological society, Norway] nr 9, desember 1983, p.13.
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Found by students University of Wroclaw per Dagmara Lesiow.
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LNEG - Laboratório Nacional de Energia e Geologia, Siorminp databse ref "1285U"
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ⓘ Morón de la Frontera ?
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