KAMACITE
Class : Elements
Subclass : Metals
Crystal system : Cubic
Chemistry : Fe,Ni
Rarity : Uncommon
Kamacite is a nickel-plated iron (it contains between 5 and 7% nickel, and sometimes a little cobalt) of almost exclusively meteoritic origin. Its name comes from the Greek kamas (perch, pole) to emphasize the elongated shape of its crystals. Kamacite forms flakes and lamellar masses in intergrowth with taenite, exceptionally crystals from a few millimeters to 30 cm. Along with taenite, it is the essential component of metallic meteorites (siderites), a little pure iron sometimes completing the paragenesis. In polished plate, after acid attack, these siderites show characteristic geometric arrangements : Widmanstätten figures, which result from the regular growth of taenite around lamellae of kamacite. Kamacite and taenite are also accessory minerals of lithosiderites, meteorites composed of silicates and alloys of iron and nickel. This natural alloy constituted a resource in the manufacture of various weapons for the first men.
Main photo : Metallic meteorite (Muonionalusta, Sweden) with Widmanstätten figures © R. Tanaka
Kamacite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fake listed for this mineral species.
Hardness : 4
Density : 7.3 to 7.87
Fracture : Undetermined
Streak : Gray
TP : Opaque
RI : -
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None
Solubility : Hydrochloric acid
Magnetism : Ferromagnetic
Radioactivity : None