Skutterudite is a metallic arsenide mineral often found as distinct, sharp cubic crystals or dense granular masses. It is a significant ore of cobalt and is typically identified by its high specific gravity and association with other cobalt-nickel minerals in hydrothermal veins.
Is this skutterudite?
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 skutterudite with a known reference. Skutterudite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Skutterudite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Skutterudite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: tin-white, silver-white, gray.
- 5Look at form & habitCrystal system: isometric. Typical habit: cubic crystals, massive, granular, or compact masses.
Often confused with
Skutterudite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside skutterudite
Minerals reported to co-occur with skutterudite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Co,Ni,Fe)As₃
- Mohs hardness
- 5.5-6
- Density
- 6.1-6.9 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Isometric
- Crystal habit
- Cubic Crystals, Massive, Granular, Or Compact Masses
- Cleavage
- Distinct On {111}
- Rarity
- Uncommon
- Uses
- Collector, Ore of Cobalt, Ore of Nickel
- Host rock
- Hydrothermal Veins, Nickel-cobalt-silver Deposits
- Typical price
- $15-150 for thumbnail to cabinet specimens
Where rockhounds find skutterudite
Classic worldwide localities
- Skuterud, Norway
- Bou Azzer, Morocco
- Cobalt, Ontario, Canada
- Schneeberg, Germany
- Jachymov, Czech Republic
Field-hunting tip
Look in hydrothermal veins, nickel-cobalt-silver deposits country — that is the host setting where skutterudite typically forms. If you start seeing cobaltite, arsenopyrite, native silver in float, you are in the right ground. Field specimens usually show a cubic crystals, massive, granular, or compact masses habit, so train your eye for that shape before scanning the outcrop.






