Cuprorhodsite is a rare platinum-group mineral typically occurring as microscopic grains within massive sulfide deposits. It is most commonly identified in polished sections via reflected light microscopy or microprobe analysis due to its extreme scarcity in macroscopic sizes.
Is this cuprorhodsite?
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 cuprorhodsite with a known reference. Cuprorhodsite sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: iron black, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: microscopic grains, anhedral grains.
Often confused with
Cuprorhodsite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Cuprorhodsite is noticeably harder (Mohs 5-5.5 vs. 1.5); streak differs, so Cuprorhodsite leaves black, Braggite leaves gray.

How to tell apart: Laurite is the harder of the two (Mohs 7.5 vs. 5-5.5); streak differs, so Cuprorhodsite leaves black, Laurite leaves dark gray.
Often found alongside cuprorhodsite
Minerals reported to co-occur with cuprorhodsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu₀.₅Fe₀.₅)Rh₂S₄
- Mohs hardness
- 5-5.5
- Density
- 6.74 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic grains, anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In alluvial placers
Where rockhounds find cuprorhodsite
Classic worldwide localities
- Gusevogorskii massif, Ural Mountains (type locality), and in the Far Eastern Region, from the Chad massif, Khabarovsk Territory, on Mt. Filipp, Kamchatka, and in the Baimka placers, Chukota, Russia
- Chromwerk, Kraubath massif, Styria, Austria
Field-hunting tip
Where it forms: In alluvial placers. If you start seeing isoferroplatinum, cuproiridsite, malanite in float, you are in the right ground. Typical habit: microscopic grains, anhedral grains. Train your eye for that shape before scanning the outcrop.




