Inyoite

(repeating unit)CaB3O3(OH)5·4H2OIMA symbolIyo[1]Strunz classification6.CA.35Crystal systemMonoclinicCrystal classPrismatic (2/m)
(same H-M symbol)Space groupP21/aUnit cella = 10.63, b = 12.06
c = 8.4 [Å]; β = 114.03°; Z = 4IdentificationColourColourless, white on dehydration.Crystal habitCommonly as prismatic to tabular crystals; also in cockscomb aggregates of pseudorhombohedral crystals; coarsely spherulitic or granularCleavageGood on {001}, distinct on {010}FractureIrregular/unevenTenacityBrittleMohs scale hardness2LustreVitreousSpecific gravity1.875Optical propertiesBiaxial (−)Refractive indexnα = 1.495 nβ = 1.505 – 1.512 nγ = 1.520BirefringenceMaximum δ = 0.025DispersionWeakReferences[2][3]

Inyoite, named after Inyo County, California, where it was discovered in 1914, is a colourless monoclinic mineral. It turns white on dehydration. Its chemical formula is Ca(H4B3O7)(OH)·4H2O or CaB3O3(OH)5·4H2O.[3] Associated minerals include priceite, meyerhofferite, colemanite, hydroboracite, ulexite and gypsum.[2][3]

References

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b Mindat.org
  3. ^ a b c Handbook of Mineralogy
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