Cabriite is an extremely rare palladium-tin-copper mineral found as microscopic inclusions within copper-nickel sulfide deposits. It is best identified through reflected light microscopy or microprobe analysis within larger sulfide assemblages, as it rarely forms identifiable hand-specimen crystals.
Is this cabriite?
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 cabriite with a known reference. Cabriite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cabriite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cabriite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: pinkish-white, bright metallic.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains and inclusions within other sulfide minerals.
Often confused with
Cabriite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cabriite
Minerals reported to co-occur with cabriite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₂SnCu
- Mohs hardness
- 3.5-4
- Density
- 10.4-10.5 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains and Inclusions Within Other Sulfide Minerals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Copper-nickel Sulfide Ores in Ultramafic Rocks
- Typical price
- $100-500 per microscopic grain mount
Where rockhounds find cabriite
Classic worldwide localities
- Norilsk ore district, Russia
- Stillwater Complex, USA
- Bushveld Igneous Complex, South Africa
Field-hunting tip
Look in copper-nickel sulfide ores in ultramafic rocks country, the host setting where cabriite typically forms. If you start seeing chalcopyrite, cubanite, pentlandite in float, you are in the right ground. Field specimens usually show a anhedral grains and inclusions within other sulfide minerals habit, so train your eye for that shape before scanning the outcrop.






