Cohenite is a rare iron carbide mineral found almost exclusively in iron meteorites. It typically appears as brittle, tin-white grains or thin plates within the nickel-iron matrix of metallic meteorites, serving as a key indicator of specific thermal conditions during the formation of planetary bodies.
Is this cohenite?
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 cohenite with a known reference. Cohenite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cohenite leaves a grey-black streak.
- 3Read the lusterHold the specimen under a strong light. Cohenite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, silver-white, tin-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular, massive, plates.
Often confused with
Cohenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cohenite
Minerals reported to co-occur with cohenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe,Ni,Co)₃C
- Mohs hardness
- 5.5-6
- Density
- 7.2-7.6 g/cm³
- Streak
- Grey-black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Granular, Massive, Plates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Iron Meteorites
- Typical price
- $50-500 depending on specimen size and source meteorite
Where rockhounds find cohenite
Classic worldwide localities
- Canyon Diablo meteorite (USA)
- Magura meteorite (Slovakia)
- Sikhote-Alin meteorite (Russia)
- Cape York meteorite (Greenland)
Field-hunting tip
Look in iron meteorites country, the host setting where cohenite typically forms. If you start seeing kamacite, taenite, schreibersite in float, you are in the right ground. Field specimens usually show a granular, massive, plates habit, so train your eye for that shape before scanning the outcrop.



