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Dominant species
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Taenite
Taenite
Chemical
Formula
γ-(Ni,Fe)
Species
Native Elements
Crystal
System
Isometric
Mohs
Scale
5
Specific
Gravity
7.8-8.22
Color
metallic grayish to white
Streak
light gray
Luster
Metallic
Diaphaneity
Opaque
Cleavage
None
Fracture
Hackly fracture
Taenite (Fe,Ni) is a mineral found naturally on Earth mostly in iron meteorites. It is an alloy of iron and nickel, with nickel proportions of 20% up to 65%.

The name is derived from the Greek for "band". Taenite is a major constituent of iron meteorites. In octahedrites it is found in bands interleaving with kamacite forming Widmanst?tten patterns, whereas in ataxites it is the dominant constituent. In octahedrites a fine intermixture with kamacite can occur, which is called plessite.

Taenite is one of four known Fe-Ni meteorite minerals: The others are kamacite, tetrataenite, and antitaenite.

Properties

It is opaque with a metallic grayish to white color. The structure is isometric-hexoctahedral. Its density is around 8 g/cm3 and hardness is 5 to 5.5 on the Mohs scale. Taenite is magnetic. The crystal lattice has the c≈a= 3.582?±0.002? . The Strunz classification is I/A.08-20, while the Dana classification is 1.1.11.2 . It is a Hexoctahedral (cubic) in structure.

Meteorite Localities with this Mineral

  • Campo del Cielo crater in Argentina.
  • Henbury Meteorites Conservation Reserve in Australia.
  • Canyon Diablo in Arizona.