| Challacolloite | |
|---|---|
Honey yellow Challacolloite crystals from the famous locality of La Fossa Crater (Vulcano Island, Aeolian Islands, Sicily, Italy) | |
| General | |
| Category | Minerals |
| Formula | KPb2Cl5 |
| IMA symbol | Chc[1] |
| Strunz classification | 3.AA.55 (10th) |
| Dana classification | 11.4.2.1 |
| Crystal system | Monoclinic |
| Crystal class | 2/m - Prismatic |
| Unit cell | 878.2 ų |
| Identification | |
| Formula mass | 630.83 gm |
| Colour | Colourless to white |
| Crystal habit | Aggregate |
| Fracture | Brittle, subconchoidal fragments |
| Mohs scale hardness | 2-3 |
| Luster | Adamantine/Greasy |
| Streak | White |
| Specific gravity | 4.77 (Calculated) |
| Density | 4.77 g/cm3 (Calculated) |
| Optical properties | Biaxial (+), a=2.004, b=2.01, g=2.024, bire=0.0200 |
| Refractive index | nα = 2.004 nβ = 2.010 nγ = 2.024 |
| 2V angle | 67° (calculated) |
Challacolloite, KPb2Cl5, is a rare halide mineral. It crystallizes in the monoclinic system (with space group P21/c[2]) and occurs as white fumarolic encrustations on lava. It occurs as intergrowths with cotunnite.[3]
It was first described from a finding at the Challacollo Mine, Iquique, Chile and thereafter identified in specimens from the 1855 Mount Vesuvius eruption and from the Kudryavyivolcano in the Kuriles and also from the Satsuma-Iwojima volcano in Japan.[4] It was recognized as a valid mineral species by the IMA (International Mineralogical Association) in 2005.[4]
Artificially grown KPb2Cl5 crystals are used for lasers.[5]