Halloysite
| Halloysite | |
|---|---|
| General | |
| Category | Phyllosilicates Kaolinite-serpentine group |
| Formula | Al2Si2O5(OH)4 |
| Strunz classification | 9.ED.10 |
| Crystal system | Monoclinic |
| Crystal class | Domatic (m) (same H-M symbol) |
| Space group | Cc |
| Unit cell | a = 5.14, b = 8.9, c = 7.214 [Å]; β = 99.7°; Z = 1 |
| Identification | |
| Color | White; grey, green, blue, yellow, red from included impurities. |
| Crystal habit | Spherical clusters, massive |
| Cleavage | Probable on {001} |
| Fracture | Conchoidal |
| Mohs scale hardness | 2–2.5 |
| Luster | Pearly, waxy, or dull |
| Diaphaneity | Semitransparent |
| Specific gravity | 2–2.65 |
| Optical properties | Biaxial |
| Refractive index | nα = 1.553–1.565 nβ = 1.559–1.569 nγ = 1.560–1.570 |
| Birefringence | δ = 0.007 |
| References | |
Halloysite is an aluminosilicate clay mineral with the empirical formula Al2Si2O5(OH)4. Its main constituents are oxygen (55.78%), silicon (21.76%), aluminium (20.90%), and hydrogen (1.56%). It is a member of the kaolinite group. Halloysite typically forms by hydrothermal alteration of alumino-silicate minerals. It can occur intermixed with dickite, kaolinite, montmorillonite and other clay minerals. X-ray diffraction studies are required for positive identification. It was first described in 1826, and subsequently named after, the Belgian geologist Omalius d'Halloy.