Libethenite

(repeating unit)Cu2PO4OHIMA symbolLib[1]Strunz classification8.BB.30Crystal systemOrthorhombicCrystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)Space groupPnnmIdentificationColorLight to dark green, blackish green, olive-greenCrystal habitGlobular, druzy, slender prismaticCleavageIndistinct on [100] and [010]FractureIrregular, uneven to conchoidalTenacityBrittleMohs scale hardness4LusterVitreous, greasyStreaklight greenSpecific gravity3.6 – 4, Average = 3.8Optical propertiesBiaxial (−)Refractive indexnα = 1.701 – 1.704 nβ = 1.743 – 1.747 nγ = 1.787 – 1.790References[2][3]

Libethenite is a rare copper phosphate hydroxide mineral. It forms striking, dark green orthorhombic crystals. It was discovered in 1823 in Ľubietová, Slovakia and is named after the German name of that locality (Libethen).[2][3] Libethenite has also been found in the Miguel Vacas Mine, Conceição, Vila Viçosa, Évora District, Portugal, and in Tier des Carrières, Cahai, Vielsaim, Stavelot Massif, Luxembourg Province, Belgium.[3]

Appearance

Detail of gemmy, emerald-green, orthorhombic libethenite microcrystals on malachite, from the type locality, Ľubietová, Slovakia. See File:Libethenite-258236.jpg for the full specimen.

Libethenite almost always takes the form of dark-green orthorhombic crystals.[2][3] It is often found in clusters with other libethenite crystals.

Formation

Libethenite is found in the oxidized zone of copper ore deposits.[3] It is most often formed from the weathering of phosphate rocks such as apatite, monazite, and xenotime.[3] There have been no confirmed findings of primary libethenite, although a probable case has been reported.[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 c http://webmineral.com/data/Libethenite.shtml Webmineral
  3. ^ a b c d e f g http://www.mindat.org/min-2394.html Mindat
Wikimedia Commons has media related to Libethenite.


  • v
  • t
  • e