Camérolaite is a very rare secondary copper sulfate-carbonate mineral typically occurring as fragile, pearly blue crusts or tiny platy aggregates. It is primarily found in the oxidized zones of copper-rich sulfide deposits. Because of its rarity and delicate nature, it is highly sought after by advanced micromount and mineral species collectors.
Is this camérolaite?
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 camérolaite with a known reference. Camérolaite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Camérolaite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Camérolaite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: blue, pale blue.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, crusts.
Often confused with
Camérolaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside camérolaite
Minerals reported to co-occur with camérolaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄Al₂(OH)₁₂(SO₄)(CO₃)·2H₂O
- Mohs hardness
- 2
- Density
- 2.8 g/cm³
- Streak
- Pale Blue
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Copper Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find camérolaite
Classic worldwide localities
- Cap Garonne mine, France
- Kamareza mine, Greece
Field-hunting tip
Look in oxidized hydrothermal copper deposits country — that is the host setting where camérolaite typically forms. If you start seeing brochantite, garnierite, malachite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




