Padmaite is a very rare palladium bismuth selenide mineral that typically occurs as microscopic grains within ore bodies. It is primarily identified through electron microprobe analysis due to its minute size and complex association with other platinum-group minerals.
Is this padmaite?
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 padmaite with a known reference. Padmaite sits at Mohs 3-4, 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: yellow.
- 4Look at form & habitCrystal system: cubic. Typical habit: grains.
Often confused with
Padmaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside padmaite
Minerals reported to co-occur with padmaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdBiSe
- Mohs hardness
- 3-4
- Density
- 9.86 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Grains
- Cleavage
- Imperfect along two perpendicular directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In metasomatic rocks in shungite-bearing metashales (Russia); in hydrothermally altered (sericitization, silicification, with minor K-metasomatism) granite-related mylonite (Brazil)
Where rockhounds find padmaite
Classic worldwide localities
- Padma River, southern Karelia, Russia (type locality)
- Buraco do Ouro gold mine, Cavalcante, Goiás State, Central Brazil
- Jinchuan intrusion, northern China
Field-hunting tip
Where it forms: In metasomatic rocks in shungite-bearing metashales (Russia); in hydrothermally altered (sericitization, silicification, with minor K-metasomatism) granite-related mylonite (Brazil). If you start seeing clausthalite, paraguanajuatite, bohdanowiczite in float, you are in the right ground. Typical habit: grains. Train your eye for that shape before scanning the outcrop.








