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.

Hardness
4
Mohs
Luster
Metallic
Streak
Gray
Transparency
Opaque

Is this kamacite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch kamacite with a known reference. Kamacite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: gray.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: steel gray, iron black.
  • 5
    Look at form & habit
    Crystal 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
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.

More kamacite photos

  • Crossing kamacite lamellae, Carlton meteorite, Texas
  • Etched Gibeon meteorite slice, kamacite pattern across the face

Common questions

How do you identify kamacite?+
Mohs hardness is 4. Luster: metallic. The streak is gray. Common colors include steel gray, iron black.
Where is kamacite found?+
Notable localities include Iron meteorites; Blaafjeld, Disko Island, Greenland (terrestrial); Bühl, near Weimar, Germany (terrestrial); Putorana Plateau, Taimyr Peninsula, Russia (terrestrial).
Is kamacite safe to handle?+
Kamacite contains nickel. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like kamacite?+
Kamacite is most often confused with Taenite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kamacite?+
Kamacite commonly co-occurs with Taenite, Graphite, Cohenite, Moissanite, Schreibersite, Troilite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kamacite form in?+
Where it forms: A major constituent of iron meteorites and present in most other meteorites. Working float back to the host body is the standard way to chase a fresh occurrence.

Find kamacite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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