Arsenopalladinite is an extremely rare palladium arsenide that typically occurs as small, metallic grains within mineralized zones. It is most often identified through micro-analysis in advanced collections due to its scarcity and similarity to other platinum-group minerals.
Is this arsenopalladinite?
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 arsenopalladinite with a known reference. Arsenopalladinite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arsenopalladinite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Arsenopalladinite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, light yellow, gray.
- 5Look at form & habitCrystal system: triclinic. Typical habit: granular, anhedral masses.
Often confused with
Arsenopalladinite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arsenopalladinite
Minerals reported to co-occur with arsenopalladinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₈(As,Sb)₃
- Mohs hardness
- 3.5
- Density
- 9.94 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Granular, Anhedral Masses
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Iron Formations
- Typical price
- $100-500 per micro-specimen
Where rockhounds find arsenopalladinite
Classic worldwide localities
- Itabira, Minas Gerais, Brazil
- Stillwater Complex, Montana, USA
Field-hunting tip
Look in hydrothermal veins in iron formations country — that is the host setting where arsenopalladinite typically forms. If you start seeing potarite, palladium, gold in float, you are in the right ground. Field specimens usually show a granular, anhedral masses habit, so train your eye for that shape before scanning the outcrop.






