Arsenudinaite is an extremely rare palladium arsenide mineral typically found in high-temperature volcanic fumarole environments. It usually occurs as microscopic grains or small aggregates and is primarily identified through advanced analytical techniques due to its extreme scarcity.
Is this arsenudinaite?
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 arsenudinaite with a known reference. Arsenudinaite 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. Arsenudinaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Arsenudinaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, pale gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive, granular.
Often confused with
Arsenudinaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arsenudinaite
Minerals reported to co-occur with arsenudinaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- As₂Pd₃
- Mohs hardness
- 3.5-4
- Density
- 6.8-7.2 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Distinct in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Volcanic Deposits
- Typical price
- $100-500 for small micro-mounts
Where rockhounds find arsenudinaite
Classic worldwide localities
- Arsenatnaya fumarole, Tolbachik Volcano, Kamchatka, Russia
Field-hunting tip
Look in fumarolic volcanic deposits country — that is the host setting where arsenudinaite typically forms. If you start seeing sopcheite, temagamite, palladseite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.




