Halotrichite
Halotrichite | |
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A sample of Halotrichite | |
General | |
Category | Sulfate minerals |
Formula (repeating unit) | FeAl2(SO4)4·22H2O. |
Strunz classification | 07.CB.85 |
Crystal symmetry |
Monoclinic sphenoidal H-M symbol: (2) Space group: P 2 |
Unit cell | a = 20.51 Å, b = 24.29 Å, c = 6.18 Å; β = 100.99°; Z=4 |
Identification | |
Color | Colorless to white, yellowish, greenish |
Crystal habit | Acicular to asbestiform clusters, incrustations and efflorescences |
Crystal system | Monoclinic |
Cleavage | Poor on {010} |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 1.5 - 2 |
Luster | Vitreous |
Diaphaneity | Transparent, translucent |
Specific gravity | 1.89 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.480 nβ = 1.486 nγ = 1.490 |
Birefringence | δ = 0.010 |
2V angle | Measured: 35° |
Solubility | Soluble in water |
Other characteristics | Astringent taste |
References | [1][2][3] |
Halotrichite, also known as feather alum, is a highly hydrated sulfate of aluminium and iron. Its chemical formula is FeAl2(SO4)4·22H2O. It forms fibrous monoclinic crystals. The crystals are water-soluble.
It is formed by the weathering and decomposition of pyrite commonly near or in volcanic vents. The locations of natural occurrences include: the Atacama Desert, Chile; Dresden in Saxony, Germany; San Juan County, Utah; Iceland and Mont Saint-Hilaire, Canada.
The name is from Latin: halotrichum for salt hair which accurately describes the precipitate/evaporite mineral.[3]
References
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