Rhodarsenide is a rare rhodium arsenide mineral that occurs primarily as small, metallic grains within platinum-group mineral assemblages. It is most frequently found in alluvial deposits derived from ultramafic rocks or in chromitite layers. Collectors prize it as a micro-mineral due to its extreme scarcity and association with platinum-group elements.
Is this rhodarsenide?
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 rhodarsenide with a known reference. Rhodarsenide sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rhodarsenide leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Rhodarsenide typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, silver-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular.
Often confused with
Rhodarsenide vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rhodarsenide
Minerals reported to co-occur with rhodarsenide. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Rh₂As
- Mohs hardness
- 3
- Density
- 11.32 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Rocks
Where rockhounds find rhodarsenide
Classic worldwide localities
- Kandagubai, India
- Itabira, Brazil
- Miass, Russia
Field-hunting tip
Look in ultramafic rocks country, the host setting where rhodarsenide typically forms. If you start seeing magnetite, chromite, gold in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.






