Poitevinite is a rare copper iron sulfate that typically forms as a secondary mineral in the oxidized zones of copper deposits. It is most often found as efflorescent crusts or small crystalline coatings rather than large crystals, making it a challenging and prized specimen for collectors of rare sulfates.
Is this poitevinite?
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 poitevinite with a known reference. Poitevinite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: pink, light red.
- 5Look at form & habitCrystal system: triclinic. Typical habit: powdery.
Often confused with
Poitevinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside poitevinite
Minerals reported to co-occur with poitevinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuSO₄·H₂O
- Mohs hardness
- 3-3.5
- Density
- 3.30 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Powdery
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in the oxidized zone of a base-metal hydrothermal mineral prospect
Where rockhounds find poitevinite
Classic worldwide localities
- Avoca claim, Hat Creek, Bonaparte River area, Lillooet district, British Columbia, Canada
Field-hunting tip
Where it forms: A rare secondary mineral in the oxidized zone of a base-metal hydrothermal mineral prospect. If you start seeing quartz, gypsum, pyrite in float, you are in the right ground. Typical habit: powdery. Train your eye for that shape before scanning the outcrop.






