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Scottyite
This page kindly sponsored by Michael Scott
| Formula: |
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| System: | Orthorhombic | |||||||||||||||
| Name: | Named for Michael Scott (1945 - ), first CEO of Apple and significant sponsor of the Rruff project. | |||||||||||||||
Also known as a synthetic phase.
Classification of Scottyite | ||||||||||||||||||||||||||||
| IMA status: | Approved 2012 | |||||||||||||||||||||||||||
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| mindat.org URL: | http://www.mindat.org/min-42861.html Please feel free to link to this page. | |||||||||||||||||||||||||||
Type Occurrence of Scottyite | ||||||||||||||||||||||||||||
| Type Locality: | Wessels Mine (Wessel's Mine), Hotazel, Kalahari manganese fields, Northern Cape Province, South Africa | |||||||||||||||||||||||||||
| General Appearance of Type Material: | Blue massive, associated with | |||||||||||||||||||||||||||
| Place of Conservation of Type Material: | Mineral Museum of the University of Arizona, Tucson, Arizona, USA, catalogue number 19334 | |||||||||||||||||||||||||||
Crystallography of Scottyite | ||||||||||||||||||||||||||||
| Crystal System: | Orthorhombic | |||||||||||||||||||||||||||
| Cell Parameters: | a = 6.8556(2) Å, b = 13.1725(4) Å, c = 6.8901(2) Å α = 90°, β = 90°, γ = 90° | |||||||||||||||||||||||||||
| Ratio: | a:b:c = 0.52 : 1 : 0.523 | |||||||||||||||||||||||||||
| Unit Cell Volume: | V 622.21 ų | |||||||||||||||||||||||||||
| X-Ray Powder Diffraction: |
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Chemical Properties of Scottyite | ||||||||||||||||||||||||||||
| Formula: |
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| Essential elements: | Ba, Cu, O, Si | |||||||||||||||||||||||||||
| All elements listed in formula: | Ba, Cu, O, Si | |||||||||||||||||||||||||||
Other Names for Scottyite | ||||||||||||||||||||||||||||
| Synonyms: |
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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 Scottyite | ||||||||||||||||||||||||||||
| Reference List: - + | Janczak, J., Kubiak, R. & Glowiak, T. (1990): Structure of barium copper pyrosilicate at 300 K. Acta Crystallographica, C46, 1383-1385. Hentschel, G. (1993): Die Lavaströme der Graulai: eine neue Fundstelle in der Westeifel. Lapis 12 (9), 11-23. (in German) [as Unnamed (Ba-Cu Silicate) identical with synthetic BaCu2Si2O7] Yamada, T., Hiroi, Z. & Takano, M. (2001): Spin-1/2 quantum antiferromagnetic chains with tunable superexchange interactions found in BaCu2(Si1-xGex)2O7. Journal of Solid State Chemistry 156, 101-109. G. Blass, H.-W. Graf, U. Kolitsch and D. Sebold (2009): The new finds from the volcanic Eifel (II). Mineralien-Welt 20 (2), 38-49. (in German) [as Unnamed (Ba-Cu Silicate) identical with synthetic BaCu2Si2O7] Yang, H., Downs, R.T., Evans, S.H., Pinch, W.W. and Origlieri, M.J. (2012): Scottyite, IMA 2012-027. CNMNC Newsletter No. 14, October 2012, page 1284; Mineralogical Magazine, 76, 1281-1288. | |||||||||||||||||||||||||||
Internet Links for Scottyite | ||||||||||||||||||||||||||||
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| Specimens: | The following Scottyite specimens are currently listed for sale on minfind.com. | |||||||||||||||||||||||||||
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Localities for Scottyite | ||||||||||||||||||||||||||||
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The map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the
symbol to view information about a locality.
The symbol next to localities in the list
can be used to jump to that position on the map.
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(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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Locality Updated: Trübenbach, Gaming, Mostviertel, Lower Austria, AustriaFrom Harald Schillhammer, 23rd May 2013 08:47:24

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