Optical Properties
| Colour Pleochroism |
usually colourless non pleochroic in thin section |
Form | small euhedral to subhedral elongate prismatic crystals with hexagonal cross sections are most common, also found as anhedral grains and granular or columnar aggregates |
| Relief/ RI |
moderate high positive nw = 1.633-1.667 ne = 1.629-1.665 |
Cleavage | poor basal and prismatic, not readily visible in thin section |
| Birefringence Interference Colours |
0.001 - 0.007 first order grey |
Twinning | rare |
| Interference Figure Optic Sign 2V |
uniaxial negative |
Optic Orientation | elongate sections show parallel extinction and are length fast |
| Composition | widest variation in composition is associated with the hydroxyl site, e.g. F for OH for Cl | Alteration | stable in most geologic environments |
| Occurrence | present as an accessory in a wide variety of igneous and metamorphic rocks and as detrital grains in sedimentary rocks | Distinguishing Features | moderate to high relief, low birefringence and uniaxial character |