Anhydrite

Orthorhombic  Images    

   
   
  Formula CaSO4
  Optic class & sign Biaxial positive
  Optical orientation X = b, Y = a, Z = c
  Optical plane (100)
  Relief Moderate-positive
  Refractive indices nx = 1.567 -1.574
ny = 1.574 -1.579
nz = 1.609 -1.618
-
  Birefringence   (max.)0.040  - 0.044
   -
  Optic Angle 2Vx
2Vz = 42 - 44°
  Sign of elongation Length-slow, l (+) or length-fast, l (-), if elongate parallel a; length-slow, l (+) if elongate parallel c
  Interference figure (001) sections display centred acute bisectrix figures with multiple isochromes
  Colour /   pleochroism Colourless
  Zoning 

  Form  Habit Massive aggregates, granular, blocky, parallel or radiating fibres, tabular
  Surface Anhedral to subhedral in aggregates; euhedral as singular crystals
  Cleavage {010} perfect, {100} very good, {001} good; all orthogonal to each other
  Twinning Simple and multiple on {011}
  Extinction Straight to traces of {001}, {100}, {010} faces and cleavages in all sections parallel to a, b, or c

  Reaction textures  Pseudomorphs after gypsum, also after calcite
  Alteration /   decomposition Gypsum

  Occurence     Ign 
  Met 
  Sed Evaporite deposits; may occur as an accessory mineral in dolomites and limestones; also in calcrete
  Hyd Oxidized zone of sulfide deposits, amygdule filling in basalts and andesites, in deposits around fumaroles and volcanic vents; in seafloor hydrothermal chimneys
  Other 

  Distinctive   properties               Low birefringence, characteristic cleavages, relief
  Additional   comments