Owensite is a rare copper-iron-nickel tin sulfide mineral characterized by its metallic luster and brassy coloration. It is primarily found as microscopic anhedral grains associated with other sulfide minerals in hydrothermal systems. Collectors typically identify this mineral through micro-analysis, as it is seldom found in macro-crystalline form.
Is this owensite?
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 owensite with a known reference. Owensite sits at Mohs 3.5, 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: black.
- 4Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Owensite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside owensite
Minerals reported to co-occur with owensite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ba,Pb)₆(Cu,Fe,Ni)₂₅S₂₇
- Mohs hardness
- 3.5
- Density
- 4.78 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral grains
- Rarity
- Rare
- Uses
- Collector
- Host rock
- All rights reserved
Where rockhounds find owensite
Classic worldwide localities
- The Wellgreen Cu-Ni-Pt deposit, Kluane District, Yukon Territory, Canada (type locality)
Field-hunting tip
Where it forms: All rights reserved. If you start seeing chalcopyrite, bornite, galena in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.





