Palladodymite is a rare palladium arsenide typically found in trace amounts within platinum-group element (PGE) deposits. It usually occurs as microscopic grains within ore minerals and is highly sought after by advanced systematic collectors of platinum-group minerals.
Is this palladodymite?
3-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 palladodymite with a known reference. Palladodymite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: white, light gray.
- 3Look at form & habitCrystal system: orthorhombic. Typical habit: inclusions, microscopic crystals.
Often confused with
Palladodymite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside palladodymite
Minerals reported to co-occur with palladodymite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₂As
- Mohs hardness
- ~5
- Density
- 11.3 g/cm³
- Colors
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Inclusions, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a small fluvial placer deposit (Russia, Zimbabwe); in chromitite xenoliths in ultramafic pipes (South Africa)
Where rockhounds find palladodymite
Classic worldwide localities
- Upper Miass River, southern Urals, Russia
- Onverwacht and Tweefontein ultramafic pipes, eastern Bushveld Complex, South Africa
- Umsweswe River sediment, Zimbabwe
Field-hunting tip
Where it forms: In a small fluvial placer deposit (Russia, Zimbabwe); in chromitite xenoliths in ultramafic pipes (South Africa). If you start seeing ruthenium, isoferroplatinum, cherepanovite in float, you are in the right ground. Typical habit: inclusions, microscopic crystals. Train your eye for that shape before scanning the outcrop.







