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, 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.






