Willyamite is a very rare member of the cobaltite group, found primarily in hydrothermal ore deposits. It typically appears as massive or granular metallic aggregates that are difficult to distinguish from other sulfosalt minerals without chemical analysis.
Is this willyamite?
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 willyamite with a known reference. Willyamite 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: steel gray, silver white.
- 5Look at form & habitCrystal system: cubic. Typical habit: pseudo cubic.
Often confused with
Willyamite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside willyamite
Minerals reported to co-occur with willyamite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Co(SbS)
- Mohs hardness
- 5-5.5
- Density
- 6.76 g/cm³
- Colors
- Streak
- Grayish black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Pseudo cubic
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In calcite–siderite veins
Where rockhounds find willyamite
Classic worldwide localities
- Consols lode, Broken Hill, Willyama Township, New South Wales, Australia
Field-hunting tip
Where it forms: In calcite–siderite veins. If you start seeing dyscrasite, costibite, calcite in float, you are in the right ground. Typical habit: pseudo cubic. Train your eye for that shape before scanning the outcrop.







