|Crystal class||Dipyramidal (mmm) |
H-M symbol: (2/m 2/m 2/m)
|Color||Light to dark green, blackish green, olive-green|
|Crystal habit||Globular, druzy, slender prismatic|
|Cleavage||Indistinct on  and |
|Fracture||Irregular, uneven to conchoidal|
|Mohs scale hardness||4|
|Specific gravity||3.6 - 4, Average = 3.8|
|Optical properties||Biaxial (-)|
|Refractive index||nα = 1.701 - 1.704 nβ = 1.743 - 1.747 nγ = 1.787 - 1.790|
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). 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.
Libethenite is found in the oxidized zone of copper ore deposits. It is most often formed from the weathering of phosphate rocks such as apatite, monazite, and xenotime. There have been no confirmed findings of primary libethenite, although a probable case has been reported.
|Wikimedia Commons has media related to Libethenite.|
|This article about a specific phosphate mineral is a stub. You can help Wikipedia by expanding it.|