Cornwallite
| Cornwallite | |
|---|---|
| Cornwallite in a vug from Pastrana, Murcia, Spain (size: 4.3 × 3.7 × 2.2 cm) | |
| General | |
| Category | Arsenate mineral | 
| Formula | Cu5(AsO4)2(OH)4 | 
| IMA symbol | Cnw | 
| Strunz classification | 8.BD.05 | 
| Dana classification | 41.4.2.2 | 
| Crystal system | Monoclinic | 
| Crystal class | Prismatic (2/m) (same H-M symbol) | 
| Space group | P21/c | 
| Unit cell | a = 17.33 Å, b = 5.82 Å, c = 4.60 Å; β = 92.22°; Z = 2 | 
| Identification | |
| Color | Verdigis green, blackish-green, emerald-green | 
| Crystal habit | Microcrystalline radial fibrous, botryoidal to globular crusts | 
| Cleavage | Distinct in one direction | 
| Fracture | Conchoidal | 
| Tenacity | Brittle | 
| Mohs scale hardness | 4.5 | 
| Luster | Sub-vitreous, resinous, waxy | 
| Streak | Apple green | 
| Diaphaneity | Translucent to opaque | 
| Specific gravity | 4.17 | 
| Optical properties | Biaxial (+/−) | 
| Refractive index | nα = 1.810 – 1.820 nβ = 1.815 – 1.860 nγ = 1.850 – 1.880 | 
| Birefringence | δ = 0.040 – 0.060 | 
| 2V angle | Measured: 30° to 50° | 
| References | |
Cornwallite is an uncommon copper arsenate mineral with formula Cu5(AsO4)2(OH)4. It forms a series with the phosphate pseudomalachite and is a dimorph of the triclinic cornubite. It is a green monoclinic mineral which forms as radial to fibrous encrustations.