Szomolnokite

Szomolnokite (Fe2+SO4 · H2O) is a monoclinic iron sulfate mineral forming a complete solid solution with magnesium end-member kieserite (MgSO4 · H2O).[1] In 1877 szomolnokite’s name was derived by Joseph Krenner from its type locality of oxidized sulfide ore containing iron in Szomolnok, Slovakia (what used to be Hungary).[1][2][3]

Szomolnokite
General
CategorySulfate mineral
Formula
(repeating unit)
Fe2+SO4 · H2O
Strunz classification7.CB.05
Dana classification29.6.2.2
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
Identification
ColorSulfur-yellow, yellow-brown, red-brown, blue, colorless
Crystal habitBipyramidal, distorted, tabular, parallel growths, globular, stalactites
FractureConchoidal to sub-conchoidal, uneven
TenacityBrittle
Mohs scale hardness2.5
LusterVitreous
DiaphaneityTranslucent
Specific gravity3.03–3.07
Density3.03–3.07 (measured), 3.10 (calculated)
Optical propertiesBiaxial (+), colorless (transmitted light)
2V angle80° (measured), 86° (calculated)
References[1][2][3]

As of mid-January 2020 the only continent on which szomolnokite has not been found and reported is Antarctica.[1]

References

Bibliography

  • Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 479-480.
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