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Spodiosite
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| Name: | From the Greek σποδιος, "spodios", ash-gray, referring to its color. | ||
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| A Mixture Of: | Calcite, Fluorapatite, Serpentine Group | ||
Originally reported from Kran Mine, Nyttsta ore field, Filipstad, Värmland, Sweden.
Classification of Spodiosite | ||||||||
| IMA status: | Discredited 2003 | |||||||
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| Dana 8th edition ID: | 41.6.11.1 41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN 6 : A2(XO4)Zq | |||||||
| mindat.org URL: | http://www.mindat.org/min-3732.html Please feel free to link to this page. | |||||||
Other Names for Spodiosite | ||||||||
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Other Information | ||||||||
| Health Warning: | No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care. | |||||||
References for Spodiosite | ||||||||
| Reference List: - + | Tiberg (1872) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 1: 84. Sjögren (1885) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 7: 666. Nordenskiöld (1893) Geologiska Föeningens I Stockholm. Förhandlinger, Stockholm: 15: 460. Cameron and McCaughey (1911) Journal of Physical Chemistry: 15: 463. Larsen, E.S. (1921) The Microscopic Determination of the Nonopaque Minerals, First edition, USGS Bulletin 679: 136. Strunz (1939) Naturwiss.: 27: 423. Palache, Charles, Harry Berman & Clifford Frondel (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana Yale University 1837-1892, Seventh edition, Volume II: 848. Mineralogical Magazine (1953): 30: 166. Holtstam, D. (2004): Spodiosite discredited. GFF 126, 253-254. | |||||||
Internet Links for Spodiosite | ||||||||
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Localities for Spodiosite | ||||||||
(TL) indicates type locality. ? indicates mineral may be doubtful at this locality. All other localities listed without reference should be considered as uncertain and unproven until references can be found.
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New Locality Added: Lägern (Otelfingen; Boppelsen), Limmattal, Zürich, SwitzerlandFrom Richard Muster, 19th Jun 2013 20:38:43















