Fluorapophyllite | |
Chemical Formula |
KCa4Si8O20(F,OH)·8(H2O) |
Species |
Silicates |
Crystal System |
Tetragonal |
Mohs Scale |
4.5-5 |
Specific Gravity |
2.33-2.37 |
Color |
Colorless, white, pink, pale, yellow, green; in thin section, colorless |
Luster |
Vitreous, pearly on {001} |
Refractive Index |
nω = 1.530 - 1.536 nε = 1.532 - 1.538 |
Diaphaneity |
Transparent to translucent |
Cleavage |
Perfect on , imperfect on |
Fracture |
Uneven |
Crystal Habit:Tabular to prismatic crystals; may be pseudocubic |
Fluorapophyllite crystallizes in the tetragonal crystal system. Tetragonal minerals have three axes of different lengths and angles of 90 degrees. Fluorapophyllite is an anisotropic mineral and has low relief. This mineral belongs to the Uniaxial (+) optical class, which means its indicatrix has a prolate sphenoid shape with a circular section, principal section, and one optic axis.
Among the apophyllite group, fluorapophyllite is the most abundant compared to the other two minerals in the group, hydroxyapophyllite and natroapophyllite. It is popular among many mineral collectors because of the large, well-developed crystals they form and the multiple colors they come in. The most wanted variation of fluorapophyllite is the green colored variant, which is found in India. Fluorapophyllite is also found in New Jersey of the United States. This mineral is found as a secondary mineral in cavities of igneous rocks such as basalt.