Crerarite is an extremely rare platinum-group mineral found as tiny inclusions or irregular aggregates within massive sulfides. It is primarily identified through electron microprobe analysis given its microscopic habit and similarity to other opaque metallic minerals.
Is this crerarite?
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 crerarite with a known reference. Crerarite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Crerarite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Crerarite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: cubic. Typical habit: microcrystalline aggregates.
Often confused with
Crerarite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside crerarite
Minerals reported to co-occur with crerarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Pt,Pb)Bi₃(S,Se)₄
- Mohs hardness
- 3.5
- Density
- 9.43 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microcrystalline Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Platinum-group Mineral Deposits
- Typical price
- n/a
Where rockhounds find crerarite
Classic worldwide localities
- Crerar Mine, Ontario, Canada
Field-hunting tip
Look in hydrothermal platinum-group mineral deposits country — that is the host setting where crerarite typically forms. If you start seeing sperrylite, chalcopyrite, pyrrhotite in float, you are in the right ground. Field specimens usually show a microcrystalline aggregates habit, so train your eye for that shape before scanning the outcrop.




