Kamacite is the iron-nickel alloy that is a major constituent of iron meteorites, typically about 90 to 95 percent iron. The IMA treats it as a nickel-rich variety of native iron rather than a separate species. In octahedrite meteorites it forms bands interleaved with taenite, producing the Widmanstätten pattern seen on etched slices. It is steel-gray to iron-black, metallic and magnetic, with a hardness of about 4 and a density near 7.9 g/cm³. The Handbook of Mineralogy also lists rare occurrences in rocks on Earth, including Disko Island, Greenland.
Is this kamacite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch kamacite with a known reference. Kamacite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: steel gray, iron black.
- 5Look at form & habitCrystal system: cubic. Typical habit: plates and lamellar masses; bands in Widmanstätten patterns.
Often confused with
Kamacite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kamacite
Minerals reported to co-occur with kamacite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- α-(Fe,Ni)
- Mohs hardness
- 4
- Density
- 7.9 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Plates and lamellar masses; bands in Widmanstätten patterns
- Cleavage
- Indistinct
- Host rock
- A major constituent of iron meteorites and present in most other meteorites
Where rockhounds find kamacite
Classic worldwide localities
- Iron meteorites
- Blaafjeld, Disko Island, Greenland (terrestrial)
- Bühl, near Weimar, Germany (terrestrial)
- Putorana Plateau, Taimyr Peninsula, Russia (terrestrial)
Field-hunting tip
Where it forms: A major constituent of iron meteorites and present in most other meteorites. If you start seeing taenite, graphite, cohenite in float, you are in the right ground. Typical habit: plates and lamellar masses; bands in Widmanstätten patterns. Train your eye for that shape before scanning the outcrop.







