Inyoite
{{Infobox mineral
| name = Inyoite
| category = Nesoborates
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| image = Inyoite-Meyerhofferite-146744.jpg
| imagesize = 260px
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| formula = CaB3O3(OH)5·4H2O
| molweight =
| strunz = 6.CA.35
| system = Monoclinic
| class = Prismatic (2/m)
(same H-M symbol)
| symmetry = P21/a
| unit cell = a = 10.63, b = 12.06
c = 8.4 [Å]; β = 114.03°; Z = 4
| colour = Colourless, white on dehydration.
| habit = Commonly as prismatic to tabular crystals; also in cockscomb aggregates of pseudorhombohedral crystals; coarsely spherulitic or granular
| twinning =
| cleavage = Good on {001}, distinct on {010}
| fracture = Irregular/uneven
| tenacity = Brittle
| mohs = 2
| lustre = Vitreous
| polish =
| refractive = nα = 1.495 nβ = 1.505 – 1.512 nγ = 1.520
| opticalprop = Biaxial (−)
| birefringence = Maximum δ = 0.025
| dispersion = Weak
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| gravity = 1.875
| density =
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| references = [http://www.mindat.org/min-2036.html Mindat.org][http://rruff.geo.arizona.edu/doclib/hom/inyoite.pdf Handbook of Mineralogy]
}}
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(H{{sub|4}}B{{sub|3}}O{{sub|7}})(OH)·4H{{sub|2}}O or CaB3O3(OH)5·4H2O. Associated minerals include priceite, meyerhofferite, colemanite, hydroboracite, ulexite and gypsum.