| Ardaite | |
|---|---|
| Ardaite associated with galena, Madjarovo polymetallic ore deposit, National Museum of Natural History, Bulgaria | |
| General | |
| Category | Sulfosalt minerals, Lead minerals |
| Formula | Pb19Sb13S35Cl7 |
| IMA symbol | Ada [1] |
| Strunz classification | 2.LB.30 (10 ed) 2/E.19-20 (8 ed) |
| Dana classification | 02.15.01.01 |
| Crystal system | Monoclinic Unknown space group |
| Identification | |
| Color | Greenish gray or bluish green |
| Mohs scale hardness | 2.5-3 |
| Luster | Metallic |
| Density | 6.44 |
| Pleochroism | Weak |
| References | Breskovska, V. V.; Mozgova, N. N.; Bortnikov, N. S.; Gorshkov, A. I.; Tzepin, A. I. (1982), "Ardaite, a new lead-antimony chlorsulphosalt" (PDF), Mineral. Mag., 46 (340): 357–361, Bibcode:1982MinM...46..357B, doi:10.1180/minmag.1982.046.340.10, S2CID 128756669 |
Ardaite is a very rare sulfosalt mineral with chemical formula Pb19Sb13S35Cl7 in the monoclinic crystal system, [2] [3] named after the Arda River, which passes through the type locality. [4]
It was discovered in 1978 and approved by the International Mineralogical Association in 1980. [5] [6] [7] It was the second well-defined natural chlorosulfosalt, after dadsonite . [8]
Greenish gray or bluish green in color, its luster is metallic. Ardaite occurs as 50 μm fine-grained aggregates of acicular crystals associated with galena, pyrostilpnite, anglesite, nadorite, and chlorine-bearing robinsonite and semseyite, in the Madjarovo polymetallic ore deposit in Bulgaria. Ardaite has a hardness of 2.5 to 3 on Mohs scale and a density of approximately 6.44. [2]
The type locality is the Madjarovo polymetallic ore deposit in the Rhodope Mountains. [9] [10] Later its occurrence was proved in the Gruvåsen deposit, near Filipstad, Bergslagen, Sweden. [6]
List of minerals recognized by the International Mineralogical Association