Samaniite is a rare copper-iron-nickel sulfide mineral found primarily in ultramafic rocks. It typically occurs as small inclusions or grains within other sulfide minerals like pentlandite and chalcopyrite, making it difficult to identify without laboratory analysis.
Is this samaniite?
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 samaniite with a known reference. Samaniite 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: bronze, yellow.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains.
Often confused with
Samaniite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside samaniite
Minerals reported to co-occur with samaniite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂Fe₅Ni₂S₈
- Mohs hardness
- 3
- Density
- 4.89 g/cm³
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Filling space between silicate minerals in lherzolites of a peridotite massif
Where rockhounds find samaniite
Classic worldwide localities
- Horoman peridotite massif, Samani-cho, Samani-gun, Hokkaido, Japan
Field-hunting tip
Where it forms: Filling space between silicate minerals in lherzolites of a peridotite massif. If you start seeing bornite, talnakhite, copper in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.







