Macdonaldite
Appearance
Macdonaldite | |
---|---|
General | |
Category | Phyllosilicate |
Formula (repeating unit) | BaCa4Si16O36(OH)2·10H2O |
Strunz classification | 9.EB.05 |
Crystal system | Orthorhombic |
Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Cmcm |
Unit cell | a = 14.06 Å, b = 23.52 Å, c = 13.08 Å; Z = 4 |
Identification | |
Color | Colorless, white |
Crystal habit | Acicular also fibrous, in radiating aggregates; granular |
Cleavage | {010} perfect, {001} good, {100} indistinct |
Mohs scale hardness | 3.5-4.0 |
Luster | Vitreous - silky |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.27 |
Optical properties | Biaxial (+/-), surface relief - low, |
Refractive index | nα = 1.518 nβ = 1.524 nγ = 1.530 |
Birefringence | 0.012 |
2V angle | Measured: 90° |
Dispersion | Weak |
References | [1][2][3][4][5] |
Macdonaldite is a rare barium silicate mineral with a chemical formula of BaCa4Si16O36(OH)2·10H2O.[6] Macdonaldite was first described in 1965 and named for Gordon A. MacDonald (1911–1978) an American volcanologist at the University of Hawaii.[6]
Macdonaldite crystallises in the orthorhombic system. Macdonaldite is anisotropic with low relief.[7]
Macdonaldite appears as veins and fracture coatings in a sanbornite and quartz bearing metamorphic rock. Macdonaldite was first described in 1965 for an occurrence near the Big Creek-Rush Creek area in Fresno County, California. It has also been reported from Mariposa and Tulare counties in California.[3][6] It has also been reported from a quarry in San Venanzo, Umbria, Italy.[3]
References
- ^ Mineralienatlas
- ^ "Macdonaldite at webmineral.com".
- ^ a b c "Macdonaldite at mindat.org".
- ^ "Macdonaldite".
- ^ Handbook of Mineralogy
- ^ a b c Alfors, J.T., Stinson, M.C., Matthews, R.A., and Pabst, A. (1965) Seven new barium minerals from eastern Fresno County, California. American Mineralogist, 50, 314-340.
- ^ Bloss, F.D. (1999) Optical Crystallography. Mineralogical Society of America, 5, 161-163.