Aubertite
Aubertite is a topic that has captured the attention of people around the world. From its discovery to its impact on society, this topic has been the subject of debate and discussion. Over the years, Aubertite has evolved and influenced different aspects of everyday life. In this article, we will explore its importance and relevance today, as well as its possible implications for the future. Without a doubt, Aubertite continues to be a topic of interest to academics, professionals and the general public, and it is essential to understand its scope and effects.
| Aubertite | |
|---|---|
 Aubertite | |
| General | |
| Category | Minerals |
| Formula | CuAl(SO4)2Cl·14H2O |
| IMA symbol | Aub |
| Crystal system | Triclinic |
| Identification | |
| Color | Azure-blue |
| Cleavage | {010} Perfect |
| Mohs scale hardness | 2-3 |
| Luster | Vitreous |
| Streak | light blue |
| Specific gravity | 1.815 |
Aubertite is a mineral with the chemical formula CuAl(SO4)2Cl·14H2O. It is colored blue. Its crystals are triclinic pedial. It is transparent. It has vitreous luster. It is not radioactive. Aubertite is rated 2-3 on the Mohs Scale. The sample was collected by J. Aubert (born 1929), assistant director, National Institute of Geophysics, France, in the year 1961. Its type locality is Queténa Mine, Toki Cu deposit, Chuquicamata District, Calama, El Loa Province, Antofagasta Region, Chile.
References
- Webmineral.com - Aubertite
- Mindat.org - Aubertite
- Handbook of Mineralogy - Aubertite
- Michael Fleischer; Joseph A. Mandarino & Adolf Pabst (1980). "New Mineral Names" (PDF). American Mineralogist. 65: 205.
- D. Ginderow & F. Cesbron (1979). "Structure cristalline de l'aubertite, AlCuCl(SO4)2.14H2O". Acta Crystallographica. B35 (11): 2499–2502. doi:10.1107/S0567740879009766.