Bornhardtite is a rare cobalt selenide mineral typically occurring as microscopic inclusions in other selenide minerals. It is best identified in laboratory settings via X-ray diffraction or electron microprobe analysis due to its visual similarity to other metallic sulfides and selenides.
Is this bornhardtite?
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 bornhardtite with a known reference. Bornhardtite sits at Mohs 4.5-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bornhardtite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Bornhardtite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: pinkish-white, gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, granular, rarely octahedral.
Often confused with
Bornhardtite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bornhardtite
Minerals reported to co-occur with bornhardtite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Co₃Se₄
- Mohs hardness
- 4.5-5
- Density
- 5.65 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Granular, Rarely Octahedral
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Selenide Deposits
- Typical price
- $50-300 per specimen depending on size and rarity
Where rockhounds find bornhardtite
Classic worldwide localities
- Tropicana mine, Australia
- Tilkerode, Germany
- Hope's Nose, England
- Skrikerum, Sweden
Field-hunting tip
Look in hydrothermal selenide deposits country, the host setting where bornhardtite typically forms. If you start seeing clausthalite, tiemannite, berzelianite in float, you are in the right ground. Field specimens usually show a massive, granular, rarely octahedral habit, so train your eye for that shape before scanning the outcrop.





