Palladosilicide is a very rare palladium silicide mineral typically occurring as microscopic grains within platinum-group element deposits. It is primarily found in association with base metal sulfides in layered mafic intrusions. Collectors usually find this species as minute inclusions within polished ore samples rather than distinct macroscopic crystals.
Is this palladosilicide?
4-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 palladosilicide with a known reference. Palladosilicide sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: silver-white, gray.
- 4Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains.
Often confused with
Palladosilicide vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside palladosilicide
Minerals reported to co-occur with palladosilicide. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₂Si
- Mohs hardness
- 5-5.5
- Density
- 9.718-9.753 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In heavy mineral concentrates from layered mafic intrusions
Where rockhounds find palladosilicide
Classic worldwide localities
- Stillwater complex, Montana, USA
- Norilsk, Russia
- Bushveld complex, South Africa
Field-hunting tip
Where it forms: In heavy mineral concentrates from layered mafic intrusions. If you start seeing chromite, pentlandite, chalcopyrite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.








