NICKELINE
Class : Sulfides and sulfosalts
Subclass : Arsenides
Crystal system : Hexagonal
Chemistry : NiAs
Rarity : Uncommon
Nickeline is a high temperature hydrothermal mineral, sometimes of magmatic origin in ultrabasic rocks. In these deposits it is commonly associated with other cobalt and nickel sulfides (gersdorffite, rammelsbergite, millerite, etc...), as well as bismuth and silver minerals. It forms a series with breithauptite (NiSb). Its name reflects is derived from the German kupfernickel (devil's copper) because this mineral does not contain any. With a metallic luster, nickeline has a very characteristic pale copper red color. Most often massive, it only occurs exceptionally in hexagonal prismatic crystals with flat or pyramidal endings. It is an accessory nickel ore, sometimes important in certain mines, such as Bou-Azzer (Morocco) or Cobalt (Ontario, Canada).
Main photo : Nickeline from Eisleben, Saxony, Germany © Vandall Thomas King
Nickeline in the World
Twinning
Twins are known on {10-11} and possible on {31-41}.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 5 to 5.5
Density : 7.78
Fracture : Conchoidal
Streak : Brown-black
TP : Opaque
RI : -
Birefringence : -
Optical character : -
Pleochroism : None
Fluorescence : None
Solubility : Aqua regia
Magnetism : ParamagneticRadioactivity : None