| Vanadiocarpholite | |
|---|---|
| General | |
| Category | Silicate mineral | 
| Formula (repeating unit) | Mn2+V3+AlSi2O6(OH)4 | 
| IMA symbol | Vcar [1] | 
| Strunz classification | 9.DB.05 | 
| Crystal system | Orthorhombic | 
| Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | 
| Space group | Ccca | 
| Unit cell | a = 13.83  Å, b = 20.681 Å c = 5.188 Å; Z = 8 | 
| Identification | |
| Color | Pale-straw yellow, honey-yellow to brown | 
| Crystal habit | Prismatic to acicular crystal clusters, vein fillings | 
| Cleavage | Perfect on {010} | 
| Tenacity | Flexible | 
| Luster | Vitreous, silky | 
| Diaphaneity | Transparent | 
| Optical properties | Biaxial (+) | 
| Refractive index | nα=1.684, nβ=1.691, nγ=1.7 | 
| Birefringence | 0.0160 | 
| References | [2] [3] | 
Vanadiocarpholite (Mn2+V3+AlSi2O6(OH)4) is straw yellow to brown silicate mineral. It crystallizes in the orthorhombic crystal system. It is the vanadium rich variety of carpholite (Mn2+Al2Si2O6(OH)4).
It was first described in 2005 for an occurrence in the Molinello Mine, Graveglia Valley, Genova Province, Liguria, Italy. [3] It occurs in chert in a manganese ore deposit as vein fillings in silicified wood. [2]
It consists of: [2]
| Manganese | 15.56% | Mn | 20.09% | MnO | 
| Aluminium | 7.64% | Al | 14.44% | Al2O3 | 
| Vanadium | 14.43% | V | 21.23% | V2O3 | 
| Silicon | 15.91% | Si | 34.04% | SiO2 | 
| Hydrogen | 1.14% | H | 10.21% | H2O | 
| Oxygen | 45.32% | O |