Rozenite
Rozenite is a hydrous iron sulfate mineral, Fe2+SO4•4(H2O).
Rozenite | |
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Rozenite from Morocco | |
General | |
Category | Sulfate mineral |
Formula (repeating unit) | Fe2+SO4•4(H2O) |
Strunz classification | 7.CB.15 |
Dana classification | 29.06.06.01 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/n |
Identification | |
Color | Colorless, white, pale green |
Crystal habit | As concretions and nodules; most commonly as powdery efflorescences or coatings on melanterite |
Mohs scale hardness | 2 - 3 |
Luster | Vitreous to dull |
Streak | White |
Diaphaneity | Semitransparent |
Specific gravity | 2.29 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.526 - 1.528 nβ = 1.536 - 1.537 nγ = 1.541 - 1.545 |
Solubility | Water soluble |
References | [1][2][3] |
It occurs as a secondary mineral, formed under low humidity at less than 21 °C (70 °F) as an alteration of copper-free melanterite, which is a post mine alteration product of pyrite or marcasite. It also occurs in lacustrine sediments and coal seams. Associated minerals include melanterite, epsomite, jarosite, gypsum, sulfur, pyrite, marcasite and limonite.[1]
It was first described in 1960 for an occurrence on Ornak Mountain, Western Tatra Mountains, Małopolskie, Poland. It was named for Polish mineralogist Zygmunt Rozen (1874–1936).[1][2]
References
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