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.

Hardness
3
Mohs
Luster
Metallic
Transparency
Opaque

Is this carletonmooreite?

4-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch carletonmooreite with a known reference. Carletonmooreite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
  • 2
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 3
    Match the color range
    Compare against the expected color range: white, silvery-white.
  • 4
    Look at form & habit
    Crystal 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
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.

Common questions

How do you identify carletonmooreite?+
Mohs hardness is 3. Luster: metallic. Common colors include white, silvery-white.
Where is carletonmooreite found?+
Notable localities include Santa Catharina meteorite; Brazil.
Is carletonmooreite safe to handle?+
Carletonmooreite contains nickel. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like carletonmooreite?+
Carletonmooreite is most often confused with Kamacite, Taenite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with carletonmooreite?+
Carletonmooreite commonly co-occurs with Low-Ni iron, Schreibersite, Nickelphosphide, Perryite, Aubréelite, Tetrataenite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does carletonmooreite form in?+
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. Working float back to the host body is the standard way to chase a fresh occurrence.
What is carletonmooreite used for?+
Carletonmooreite is used in collector.

Find carletonmooreite on the map

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