Terlinguaite

(repeating unit)Hg2ClOIMA symbolTlg[1]Strunz classification3.DD.20Crystal systemMonoclinicCrystal classPrismatic (2/m)
(same H-M symbol)Space groupC2/cUnit cella = 19.51 Å, b = 5.91 Å
c = 9.47 Å; β = 143.81°; Z = 4IdentificationColorSulfur-yellow, greenish yellow, brownCrystal habitAggregates of equant to elongated crystals, powdery, massiveCleavagePerfect on [101]TenacityBrittleMohs scale hardness2.5LusterBrilliant adamantineStreakLemon-yellow, turning olive-greenDiaphaneityTransparent to translucentSpecific gravity9.22Optical propertiesBiaxial (-)Refractive indexnα = 2.350 nβ = 2.640 nγ = 2.660Birefringenceδ = 0.310PleochroismWeak, green and yellow2V angleMeasured: 20°Alters toturns olive-green on exposure to lightReferences[2][3][4]

Terlinguaite is the naturally occurring mineral with formula Hg2ClO. It is formed by the weathering of other mercury-containing minerals. It was discovered in 1900 in the Terlingua District of Brewster County, Texas, for which it is named.[5] Its color is yellow, greenish yellow, brown, or olive green.

References

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  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. ^ Handbook of Mineralogy
  3. ^ Mindat.org
  4. ^ Webmineral data
  5. ^ Hillebrand, W. F.; Schaller, W. T. (1907). "Art. XXVI. "The Mercury Minerals from Terlingua, Texas: Kleinite, Terlinguaite, Eglestonite, Montroydite, Calomel, Mercury"". The American Journal of Science. s4-24 (139): 259–274. doi:10.2475/ajs.s4-24.141.259. Retrieved 2009-05-21.


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