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 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Haxonite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Haxonite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, silver-gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular.
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
- 6
- Density
- 7.52 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Iron Meteorites
- Typical price
- $100-500 for small research fragments
Where rockhounds find haxonite
Classic worldwide localities
- Canyon Diablo meteorite (Arizona, USA)
- Toluca meteorite (Mexico)
- Henbury meteorite (Australia)
Field-hunting tip
Look in iron meteorites country, the host setting where haxonite typically forms. If you start seeing kamacite, taenite, schreibersite in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.



