Ullmannite is a nickel antimony sulfide that typically appears as cubic or pyritohedral metallic crystals. It is primarily found in hydrothermal veins associated with other sulfide minerals and is valued by collectors for its sharp crystal habits and distinct metallic luster.
Is this ullmannite?
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 ullmannite with a known reference. Ullmannite sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: grayish black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: silver white, steel gray, tin white.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive.
Often confused with
Ullmannite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ullmannite
Minerals reported to co-occur with ullmannite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NiSbS
- Mohs hardness
- 5-5.5
- Density
- 6.65 g/cm³
- Streak
- Grayish black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive
- Cleavage
- Perfect on {001}
- Rarity
- Uncommon
- Uses
- Collector, Ore
- Host rock
- With nickel minerals in hydrothermal veins
Where rockhounds find ullmannite
Classic worldwide localities
- Friedrich mine, near Wissen, Germany
- Petersbach mine, near Eichelhardt, Germany
- Gosenbach, Germany
- Salchendorf, Germany
- Ramsbeck, Germany
- Harz Mountains, from Neudorf, Germany
Field-hunting tip
Where it forms: With nickel minerals in hydrothermal veins. If you start seeing nickeline, gersdorffite, pentlandite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.








