Haxonite is a rare iron-nickel carbide mineral that forms within iron meteorites as a result of specific cooling histories. It is typically found as microscopic grains or small inclusions intergrown with other iron-nickel phases, making it a prized discovery for meteorite specialists and researchers. Due to its extraterrestrial origin and rarity, it is almost exclusively found by analyzing cross-sections of known iron meteorite falls.
Is this haxonite?
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 haxonite with a known reference. Haxonite 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. Streak: gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: tin white.
- 5Look at form & habitCrystal system: cubic. Typical habit: microscopic crystals.
Often confused with
Haxonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside haxonite
Minerals reported to co-occur with haxonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe,Ni)₂₃C₆
- Mohs hardness
- 5.5-6
- Density
- 7.7 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In iron meteorites and carbonaceous chondrites
Where rockhounds find haxonite
Classic worldwide localities
- Toluca, Canyon Diablo, Edmonton (Kentucky), Tazewell, and many other iron meteorites, characteristic of group I and group IIIC-IIID
Field-hunting tip
Where it forms: In iron meteorites and carbonaceous chondrites. If you start seeing kamacite, taenite, schreibersite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.





