Taenite is a nickel-iron alloy found almost exclusively in iron meteorites. It forms the finer components of the Widmanstätten pattern when intergrown with kamacite and is characterized by its high nickel content, which grants it higher resistance to chemical etching than its counterpart.
Is this taenite?
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 taenite with a known reference. Taenite sits at Mohs 5-5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Taenite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Taenite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: isometric. Typical habit: massive, granular, or interstitial filling in meteorites.
Often confused with
Taenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside taenite
Minerals reported to co-occur with taenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeNi
- Mohs hardness
- 5-5.5
- Density
- 8.0-8.2 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Isometric
- Crystal habit
- Massive, Granular, Or Interstitial Filling in Meteorites
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Iron Meteorites
- Typical price
- $50-500 depending on specimen size and provenance
Where rockhounds find taenite
Classic worldwide localities
- Muonionalusta (Sweden)
- Campo del Cielo (Argentina)
- Gibeon (Namibia)
- Henbury (Australia)
- Canyon Diablo (USA)
Field-hunting tip
Look in iron meteorites country — that is the host setting where taenite typically forms. If you start seeing kamacite, troilite, schreibersite in float, you are in the right ground. Field specimens usually show a massive, granular, or interstitial filling in meteorites habit, so train your eye for that shape before scanning the outcrop.


