| Hexagonite | |
|---|---|
| | |
| General | |
| Category | mineral variety of tremolite |
| Formula | Ca 2 Mg 5 (Si 8 O 22) (OH)2 |
| Space group | monoclinic – prismatic |
| Identification | |
| Color | red to pink, lilac to purple |
| Crystal habit | elongated, bladed crystals, granula |
| Twinning | simple, multiple |
| Cleavage | [110] perfect; [010] distinct |
| Fracture | uneven |
| Tenacity | brittle |
| Mohs scale hardness | 5.0–6.0 |
| Luster | vitreous |
| Refractive index | 1.599–1.637 biaxial ( - ) |
| Birefringence | 0.019–0.028 |
| Pleochroism | bluish–red, deep rose, deep red–violet |
| Dispersion | weak, r < v |
Hexagonite is the red to pink, lilac to purple manganoan variety of tremolite. A rare amphibole, it can be transparent, translucent, and rarely opaque.
Hexagonite is pleochroic, potentially displaying varying shades of blue, violet, purple, or red. [1] It is also known as "mangan-tremolite", since the manganese imparts the mineral's unique colors.[ citation needed ] Pink, lilac, and purple are the most common colors. [1] Hexagonite has been successfully faceted. [1]
Tremolite was discovered in 1789. [2] Hexagonite, a varietal form of tremolite, has a Mohs hardness of 5.0-6.0. [3] Like tremolite, it is a calcium magnesium silicate hydroxide with the formula: Ca 2 Mg 5 (Si 8 O 22) (OH)2. [3]
The mineral was given the name, hexagonite, because its crystal structure was believed at one time to be hexagonal. Since then, however, it has been found to be monoclinic. [3]
The mineral is found primarily in the Balmat-Edwards zinc district of Edwards, St. Lawrence County, New York, United States. [4] It was also found in the Czech Republic in the Chýnov caves. [5]