Garutiite is an extremely rare nickel-iron-iridium alloy found primarily within ophiolitic chromitite complexes. Because it typically occurs as microscopic grains or inclusions within other platinum-group minerals, it is almost exclusively a specimen for advanced micromount collectors and researchers.
Is this garutiite?
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 garutiite with a known reference. Garutiite sits at Mohs 4.5-5, 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, gray, gray-black.
- 4Look at form & habitCrystal system: hexagonal. Typical habit: microscopic grains and inclusions.
Often confused with
Garutiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside garutiite
Minerals reported to co-occur with garutiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ni,Fe,Ir)
- Mohs hardness
- 4.5-5
- Density
- 11.33 g/cm³
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Microscopic grains and inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- Of probable secondary origin, formed at low temperatures during post-magmatic processes, such as serpentinization and/or lateritization
Where rockhounds find garutiite
Classic worldwide localities
- Loma Peguera, Dominican Republic
Field-hunting tip
Where it forms: Of probable secondary origin, formed at low temperatures during post-magmatic processes, such as serpentinization and/or lateritization. If you start seeing hexaferrum, ferrian chromite, chlorite-group minerals in float, you are in the right ground. Typical habit: microscopic grains and inclusions. Train your eye for that shape before scanning the outcrop.





