Ruthenarsenite is a rare ruthenium arsenide mineral typically found as small, metallic grains within platinum group mineral deposits. Collectors usually find it alongside other rare palladium and platinum minerals in specific geological settings like the Stillwater Complex. Due to its rarity, it is almost exclusively a specimen of interest for advanced mineralogists.
Is this ruthenarsenite?
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 ruthenarsenite with a known reference. Ruthenarsenite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ruthenarsenite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Ruthenarsenite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, silver-white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains, massive.
Often confused with
Ruthenarsenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ruthenarsenite
Minerals reported to co-occur with ruthenarsenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- RuAs
- Mohs hardness
- 5-6
- Density
- 9.4-9.6 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral Grains, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Igneous Complexes, Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find ruthenarsenite
Classic worldwide localities
- Musonoi mine, Democratic Republic of the Congo
- Stillwater complex, Montana, USA
Field-hunting tip
Look in ultramafic igneous complexes, hydrothermal veins country — that is the host setting where ruthenarsenite typically forms. If you start seeing sperrylite, platinum group minerals, galena in float, you are in the right ground. Field specimens usually show a anhedral grains, massive habit, so train your eye for that shape before scanning the outcrop.



