Chalcocyanite is a rare anhydrous copper sulfate that typically forms as a dehydration product of chalcanthite. It appears as pale blue crusts or powdery aggregates and is notably unstable in humid environments, as it easily absorbs water to revert to chalcanthite.
Is this chalcocyanite?
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 chalcocyanite with a known reference. Chalcocyanite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Chalcocyanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Chalcocyanite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, pale blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crusts, fibrous aggregates, massive.
Often confused with
Chalcocyanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside chalcocyanite
Minerals reported to co-occur with chalcocyanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuSO₄
- Mohs hardness
- 2.5
- Density
- 3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Crusts, Fibrous Aggregates, Massive
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumaroles and Oxidized Copper Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find chalcocyanite
Classic worldwide localities
- Vesuvius, Italy
- Chuquicamata, Chile
- Rio Tinto, Spain
- Bisbee, Arizona, USA
Field-hunting tip
Look in fumaroles and oxidized copper deposits country — that is the host setting where chalcocyanite typically forms. If you start seeing chalcanthite, copper, tenorite in float, you are in the right ground. Field specimens usually show a crusts, fibrous aggregates, massive habit, so train your eye for that shape before scanning the outcrop.





