rozenite
Sign in to saveAlso known as IMA1962-006
Rozenite is a hydrous iron sulfate mineral, Fe2+SO4·4(H2O).
In the Vinony graph
Vinony's link graph records 14 inbound references to rozenite, and connects out to Poland, Morocco and iron.
Vinony files it under Iron(II) minerals, Minerals in space group 14 and Monoclinic minerals.
Vinony links it to 10 Wikipedia language editions.
Key facts
- Mineral.name
- Rozenite
- Mineral.category
- Sulfate mineral
- Mineral.image
- Rozenit, Maroko.jpg
- Mineral.caption
- Rozenite from Morocco
- Mineral.formula
- Fe2+SO4·4(H2O)
- Mineral.IMAsymbol
- Rzn
- Mineral.strunz
- 7.CB.15
- Mineral.dana
- 29.06.06.01
- Mineral.system
- Monoclinic
- Mineral.class
- Prismatic (2/m) (same H-M symbol)
- Mineral.symmetry
- P21/n
- Mineral.color
- Colorless, white, pale green
- Mineral.habit
- As concretions and nodules; most commonly as powdery efflorescences or coatings on melanterite
- Mineral.mohs
- 2–3
- Mineral.luster
- Vitreous to dull
- Mineral.streak
- White
- Mineral.diaphaneity
- Semitransparent
- Mineral.gravity
- 2.29
via Wikipedia infobox
Wikidata facts
- Image
- Rozenit, Maroko.jpg
Show 8 more facts
- streak color
- white
- Commons category
- Rozenite
- crystal system
- monoclinic crystal system
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 7.CB.15
- Nickel-Strunz 9th edition (updated 2009)
- 7.CB.15
- IMA Mineral Symbol
- Rzn
- chemical formula
- FeSO₄ * 4H₂O
- Strunz 8th edition (series ID, updated)
- VI/C.02
via Wikidata · CC0
~1 min read
Encyclopedic overview
1 sectionsContents
- References
Rozenite is a hydrous iron sulfate mineral, Fe2+SO4·4(H2O).
It occurs as a secondary mineral, formed under low humidity at less than 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.
Excerpted from Wikipedia’s “rozenite” article, available under the CC BY-SA 4.0 licence.