Népouite

Népouite is a rare nickel silicate mineral which has the apple green color typical of such compounds. It was named by the French mining engineer Edouard Glasser in 1907 after the place where it was first described (the type locality), the Népoui Mine, Népoui, Poya Commune, North Province, New Caledonia.[5] The ideal formula is Ni₃(Si₂O₅)(OH)₄, but most specimens contain some magnesium, and (Ni,Mg)₃(Si₂O₅)(OH)₄ is more realistic. There is a similar mineral called lizardite (named after the Lizard Complex in Cornwall, England) in which all of the nickel is replaced by magnesium, formula Mg₃(Si₂O₅)(OH)₄.[6] These two minerals form a series; intermediate compositions are possible, with varying proportions of nickel to magnesium.[7]

Népouite
Népouite from the Népoui Mine, North Province, New Caledonia. Specimen size: 21 cm.
General
Category	Phyllosilicates Kaolinite-serpentine group
Formula (repeating unit)	Ni3(Si2O5)(OH)4
IMA symbol	Npo[1]
Strunz classification	9.ED.15
Dana classification	71.1.2b.3
Crystal system	Orthorhombic
Crystal class	pyramidal (mm2) (same H-M symbol)
Space group	Ccm21 (no. 36)
Identification
Color	bright green (typical of nickel bearing silicates) to yellowish or brownish green, depending on nickel content
Crystal habit	generally massive, also fibrous and microscopic pseudohexagonal platy crystals
Cleavage	perfect on {001}
Mohs scale hardness	2 to 2+1⁄2
Luster	earthy to waxy, also pearly
Streak	greenish white
Diaphaneity	semitranslucent
Specific gravity	3.18 to 3.24 (measured)
Optical properties	biaxial (-)
Refractive index	nα = 1.600 - 1.630 nγ = 1.635 - 1.650
Birefringence	0.035
Pleochroism	weak. X = green to yellow green Z = yellow-green
References	[2][3][4]

Pecoraite is another rare mineral with the same chemical formula as népouite, but a different structure; such minerals are said to be dimorphs of each other, in the same way as graphite is a dimorph of diamond. Népouite, lizardite and pecoraite are all members of the kaolinite-serpentine group.[8]

Garnierite is a green nickel ore that formed as a result of weathering of ultramafic rocks, and that occurs in many nickel deposits worldwide. It is a mixture of various nickel and magnesium phyllosilicates (sheet silicates), including népouite. Associated minerals include calcite, chlorite, goethite, halloysite, nontronite, pimelite, quartz, sepiolite, serpentine, talc and willemseite.

As well as the type locality in New Caledonia, it has been found in Australia, Austria, the Czech Republic, the Democratic Republic of Congo, Germany, Greece, Italy, Japan, Morocco,[9] Poland, Russia, South Africa and the United States.