Ruarsite is a rare ruthenium-arsenic-sulfur mineral that typically occurs as microscopic inclusions within platinum-group ore deposits. Because it is rarely found in large visible crystals, collectors usually seek out polished ore sections or matrix samples containing associated platinum-group minerals.
Is this ruarsite?
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 ruarsite with a known reference. Ruarsite 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. Ruarsite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Ruarsite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, inclusions in other minerals.
Often confused with
Ruarsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ruarsite
Minerals reported to co-occur with ruarsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- RuAsS
- Mohs hardness
- 5-6
- Density
- 9.2-9.6 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral Grains, Inclusions in Other Minerals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Rocks, Platinum-group Mineral Deposits
- Typical price
- $50-300+ depending on size and association
Where rockhounds find ruarsite
Classic worldwide localities
- Urals, Russia
- Bushveld Complex, South Africa
- Sudbury, Canada
Field-hunting tip
Look in ultramafic rocks, platinum-group mineral deposits country — that is the host setting where ruarsite typically forms. If you start seeing laurite, sperrylite, platinum-group minerals in float, you are in the right ground. Field specimens usually show a anhedral grains, inclusions in other minerals habit, so train your eye for that shape before scanning the outcrop.




