Millosevichite
| Millosevichite | |
|---|---|
| General | |
| Category | Sulfate mineral |
| Formula (repeating unit) | Al2(SO4)3 |
| Strunz classification | 07.AB.05 |
| Crystal symmetry |
Trigonal rhombohedral H-M symbol: (3) Space Group: R3 |
| Unit cell | a = 8.05 Å, c = 21.19 Å; Z=6 |
| Identification | |
| Color | Indigo, bright red, brick-red |
| Crystal habit | Granular aggregates of minute crystals; stalactitic porous masses |
| Crystal system | Trigonal |
| Mohs scale hardness | 1.5 |
| Luster | Vitreous |
| Diaphaneity | Semitransparent |
| Specific gravity | 1.72 measured |
| Optical properties | Uniaxial (+) |
| Refractive index | nω = 1.500 nε = 1.515 |
| Birefringence | δ = 0.015 |
| Other characteristics | Hygroscopic |
| References | [1][2][3] |
Millosevichite is a rare sulfate mineral with the chemical formula Al2(SO4)3.[2] Aluminium is often substituted by iron. It forms finely crystalline and often porous masses.
It was first described in 1913 for an occurrence in Grotta dell'Allume, Porto Levante, Vulcano Island, Lipari, Aeolian Islands, Sicily. It was named for Italian mineralogist Federico Millosevich (1875–1942) of the University of Rome.[1]
The mineral is mainly known from burning coal dumps, acting as one of the main minerals forming sulfate crust. It can be also found in volcanic solfatara environments.[1][4] It occurs with native sulfur, sal ammoniac, letovicite, alunogen and boussingaultite.[1]
References
- ↑ 1.0 1.1 1.2 1.3 Handbook of Mineralogy
- ↑ 2.0 2.1 Mindat
- ↑ Webmineral
- ↑ Chesnokov B. V. and Shcherbakova E. P. 1991: Mineralogiya gorelykh otvalov Chelyabinskogo ugolnogo basseina - opyt mineralogii tekhnogenesa. Nauka, Moscow