Rhomboclase | |
---|---|
General | |
Category | Sulfate mineral |
Formula (repeating unit) | H5Fe3+O2(SO4)2·2(H2O) |
IMA symbol | Rbc [1] |
Strunz classification | 7.CB.55 |
Crystal system | Orthorhombic |
Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Pnma |
Identification | |
Color | blue, colourless, white, yellow, light green, grey |
Luster | sub-Vitreous, Pearly |
Streak | white |
Diaphaneity | transparent |
References | [2] [3] |
Rhomboclase is an acidic iron sulfate mineral with a formula reported as H5Fe3+O2(SO4)2·2(H2O) [4] or HFe(SO4)2·4(H2O). [2] It crystallizes in the orthorhombic system and typically occurs as tabular crystals with a rhombic outline. [4] It occurs as transparent colorless, blue, green, yellow or grey crystals with a vitreous to pearly luster. [3]
Rhomboclase forms within the oxidizing environment of pyrite rich ore deposits and is reported as a post mine mineral of arid regions. [4]
It was first described in 1888 for an occurrence in Slovakia and was named from Latin, rhombus, rhomb, and Greek klasis, to break, for its crystal form and perfect basal cleavage. [2]
Rhomboclase | |
---|---|
General | |
Category | Sulfate mineral |
Formula (repeating unit) | H5Fe3+O2(SO4)2·2(H2O) |
IMA symbol | Rbc [1] |
Strunz classification | 7.CB.55 |
Crystal system | Orthorhombic |
Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Pnma |
Identification | |
Color | blue, colourless, white, yellow, light green, grey |
Luster | sub-Vitreous, Pearly |
Streak | white |
Diaphaneity | transparent |
References | [2] [3] |
Rhomboclase is an acidic iron sulfate mineral with a formula reported as H5Fe3+O2(SO4)2·2(H2O) [4] or HFe(SO4)2·4(H2O). [2] It crystallizes in the orthorhombic system and typically occurs as tabular crystals with a rhombic outline. [4] It occurs as transparent colorless, blue, green, yellow or grey crystals with a vitreous to pearly luster. [3]
Rhomboclase forms within the oxidizing environment of pyrite rich ore deposits and is reported as a post mine mineral of arid regions. [4]
It was first described in 1888 for an occurrence in Slovakia and was named from Latin, rhombus, rhomb, and Greek klasis, to break, for its crystal form and perfect basal cleavage. [2]