| Halotrichite | |
|---|---|
|   A sample of halotrichite | |
| General | |
| Category | Sulfate minerals | 
| Formula | FeAl2(SO4)4·22H2O | 
| IMA symbol | Hth [1] | 
| Strunz classification | 7.CB.85 | 
| Crystal system | Monoclinic | 
| Crystal class | Prismatic (2m) (same H-M symbol) | 
| Space group | P21/c | 
| Unit cell | a = 20.51, b = 24.29 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 | 
| 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 | [2] [3] [4] | 
Halotrichite, also known as feather alum, is a highly hydrated sulfate of aluminium and iron. Its chemical formula is FeAl2(SO4)2·22H2O. 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; Idrija, Slovenia; and Mont Saint-Hilaire, Canada.
The name is from Latin: halotrichum for salt hair which accurately describes the precipitate/evaporite mineral. [4]