Gypsum

Monoclinic  Images    

   
   
  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
ny = 1.522 -1.526
nz = 1.529 -1.531
-
  Birefringence   (max.)0.009  - 0.010
   -
  Optic Angle 2Vx
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 

  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.

  Reaction textures  
  Alteration /   decomposition Gypsum is itself a hydration product of anhydrite and also a weathering product of sulfides

  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 

  Distinctive   properties               Low birefringence, low negative relief, characteristic cleavages, inclined extinction
  Additional   comments