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Mineralogy Anorthite is the calcium-rich endmember of the plagioclase system, the other endmember being albite[?] (sodium-rich). The range of intermediate compositions have varying ratios of calcium and sodium ions.
Occurrence Anorthite occurs in igneous and metamorphic[?] rocks. Its type localities[?] are Monte Somma and Valle di Fassa, Italy,
| Crystallographic system | Triclinic |
| Colours | Normally colourless or white, colourless in thin section. |
| Lustre | Vitreous |
| Hardness | 6-6.5 |
| Refractive index | 1.51 |
| Cleavage | 3: 1 perfect, 1 good, 1 poor |
| Twinning | Multiple lamellar and Carlsbad twins[?] |
| Pleochroism | Yellow to dark green to transparent to opaque |
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