Sugilite
| Sugilite | |
|---|---|
Sugilite from Wessels Mine in Northern Cape Province, South Africa
|
|
| General | |
| Category | Cyclosilicate |
|
Formula (repeating unit) |
KNa2(Fe,Mn,Al)2Li3Si12O30 |
| Strunz classification | 9.CM.05 |
| Dana classification | 63.02.01a.09 |
| Crystal system | Hexagonal |
| Crystal class | Dihexagonal dipyramidal (6/mmm) H-M symbol: (6/m 2/m 2/m) |
| Space group | P6/mcc |
| Unit cell | a = 10, c = 14 [Å]; Z = 2 |
| Identification | |
| Color | Light brownish-yellow, purple, violet, reddish violet, pale pink, colorless |
| Crystal habit | Prismatic crystals, typically granular to massive |
| Cleavage | Poor on {0001} |
| Mohs scale hardness | 6–6½ |
| Luster | Vitreous |
| Streak | White |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 2.74 |
| Optical properties | Uniaxial (-) |
| Refractive index | nω = 1.610 nε = 1.607 |
| Birefringence | δ = 0.003 |
| Pleochroism | Weak |
| References | |
Sugilite (/ˈsuːɡᵻlaɪt/ SOO-gi-lyt), also known as lavulite, royal azel, cybeline, and wesselite, is a relatively rare pink to purple cyclosilicate mineral with the complex chemical formula KNa2(Fe, Mn, Al)2Li3Si12O30. Sugilite crystallizes in the hexagonal system with prismatic crystals. The crystals are rarely found and the form is usually massive. It has a Mohs hardness of 5.5 to 6.5 and a specific gravity of 2.75 to 2.80. It is mostly translucent.
Sugilite was first described in 1944 by the Japanese petrologist Ken-ichi Sugi (1901–1948) for an occurrence on Iwagi Islet, Japan, where it is found in an aegirine syenite intrusive . It is found in a similar environment at Mont Saint-Hilaire, Quebec, Canada. In the Wessels mine in Northern Cape Province of South Africa, sugilite is mined from a strata-bound manganese deposit. It is also reported from Liguria and Tuscany, Italy; New South Wales, Australia and Madhya Pradesh, India.
...
Wikipedia