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Formula | CaSO4 ∙ 2H2O |
| Optic class & sign | Biaxial positive |
| Optical orientation | X near a, Y = b, Z at a high angle to c (52°) |
| Optical plane | (010) |
| Relief | Low-negative |
| Refractive indices | nx = 1.519 -1.521
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ny = 1.522 -1.526
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nz = 1.529 -1.531
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- |
| Birefringence (max.) | 0.009 - 0.010 |
| | - |
| Optic Angle
| 2Vx
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| 2Vz
= 58° - |
| Sign of elongation | Length-slow, l (+), or length-fast, l (-), in sections at a high angle to (010); in prismatic sections, the sign of elongation is problematic to determine, due to the large ZɅc angle. |
| Interference figure | Broad and diffuse isogyres on a mid-first-order white background |
| Colour / pleochroism | Colourless |
| Zoning | |
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Form | Habit | Tabular, elongate-prismatic or acicular ∥ c, rarely ∥ a, rosettes, granular; crystals may be curved |
| | Surface | Euhedral to anhedral |
| Cleavage | {010} perfect, {100} distinct, 2 sets {111} good, intersecting at 42° and 138° |
| Twinning | Simple {100} |
| Extinction | Generally oblique; max extinction angles ZɅc and XɅc in (010) sections; sections ∥ b show straight extinction to traces of (010) cleavage and (010) crystal faces. |
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Reaction textures | |
| Alteration / decomposition | Gypsum is itself a hydration product of anhydrite and also a weathering product of sulfides |
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Occurence | Ign | |
| | Met | |
| | Sed | Evaporite deposits; secondary from hydration of anhydrite; speleothems; efflorescent in desert sand (“desert roses”) |
| | Hyd | Oxidized zone of sulfide deposits; precipitate around fumaroles and volcanic vents |
| | Other | |
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Distinctive properties | Low birefringence, low negative relief, characteristic cleavages, inclined extinction |
| Additional comments | |
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