Oosterboschite is an exceptionally rare palladium-copper selenide mineral found in the oxidation zones of specific cobalt-copper deposits. It typically occurs as microscopic grains embedded within larger mineral masses, requiring professional micro-analysis for definitive identification.
Is this oosterboschite?
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 oosterboschite with a known reference. Oosterboschite 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. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains, microscopic crystals.
Often confused with
Oosterboschite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oosterboschite
Minerals reported to co-occur with oosterboschite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Pd,Cu)₇Se₅
- Mohs hardness
- 4.5-5
- Density
- 8.48 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral grains, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- In the zone of oxidation (Musonoi mine, Congo)
Where rockhounds find oosterboschite
Classic worldwide localities
- Musonoi Cu–Co mine, near Kolwezi, Katanga Province, Congo (Shaba Province, Zaire) (type locality)
- Copper Hills prospect, East Pilbara region, Western Australia
- Hope’s Nose, Torquay, Devon, England
Field-hunting tip
Where it forms: In the zone of oxidation (Musonoi mine, Congo). If you start seeing verbeekite, trogtalite, selenian digenite in float, you are in the right ground. Typical habit: anhedral grains, microscopic crystals. Train your eye for that shape before scanning the outcrop.




