Carletonmooreite is a rare nickel silicide mineral known primarily from iron meteorites, specifically those rich in nickel. It typically occurs as minute grains intergrown with other iron-nickel phases like kamacite and taenite, making it difficult for amateur collectors to identify without professional geochemical analysis.
Is this carletonmooreite?
4-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 carletonmooreite with a known reference. Carletonmooreite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: white, silvery-white.
- 4Look at form & habitCrystal system: cubic. Typical habit: microscopic grains.
Often confused with
Carletonmooreite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside carletonmooreite
Minerals reported to co-occur with carletonmooreite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni₃Si
- Mohs hardness
- 3
- Density
- 7.89 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic grains
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Localized on plessite fields in aubrite metal nodules in a meteorite, probably formed by low-temperature epitaxial growth by solid-state diffusion from kamacite on tetrataenite
Where rockhounds find carletonmooreite
Classic worldwide localities
- Santa Catharina meteorite
- Brazil
Field-hunting tip
Where it forms: Localized on plessite fields in aubrite metal nodules in a meteorite, probably formed by low-temperature epitaxial growth by solid-state diffusion from kamacite on tetrataenite. If you start seeing low-ni iron, schreibersite, nickelphosphide in float, you are in the right ground. Typical habit: microscopic grains. Train your eye for that shape before scanning the outcrop.







