| Reference Type | Journal (article/letter/editorial) |
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| Title | On pink epsomites and fauserite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Hey, Max H. | Author |
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| Year | 1931 (June) | Volume | 22 |
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| Issue | 133 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_22/22-133-510.pdf+ |
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| DOI | doi:10.1180/minmag.1931.022.133.03 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 7118 | Long-form Identifier | mindat:1:5:7118:9 |
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| GUID | 0 |
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| Full Reference | Hey, Max H. (1931) On pink epsomites and fauserite. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (133) 510-518 doi:10.1180/minmag.1931.022.133.03 |
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| Plain Text | Hey, Max H. (1931) On pink epsomites and fauserite. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (133) 510-518 doi:10.1180/minmag.1931.022.133.03 |
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| In | (1929) Mineralogical Magazine Vol. 22 (133) Mineralogical Society |
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| Abstract/Notes | In 1865 A. Breithaupt described a new mineral from Herrengrund, Hungary, to which he gave the name of fauserite. It formed very pale pink crystalline aggregates and prismatic crystals, with prism angle near 88°42′ (over a), apparently orthorhombic, and cleavage b(010). Two other prisms with angles (over a) 54°39′ and 107° 50′ were observed, and a pyramid p, giving mp= 52° ; these would correspond to forms (210), (340), and (111), and the angles are near those of epsomite. An analysis by Mollnár gave the figures shown under I below—a magnesium and manganese sulphate hexahydrate, with the molecular ratio MgSO4(Mn,Mg)SO4 = 31.62 %. There is no evidence that the analysed material (stated to be crystalline) was homogeneous. |
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