Bonattite is a rare copper sulfate mineral that typically forms as an efflorescence in the oxidized zones of copper mines. It is characterized by its pale blue to white fibrous or crust-like habits and is usually found alongside other secondary copper minerals like chalcanthite.
Is this bonattite?
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 bonattite with a known reference. Bonattite 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. Bonattite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bonattite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, blue, pale blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, crystalline crusts, efflorescent aggregates.
Often confused with
Bonattite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bonattite
Minerals reported to co-occur with bonattite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuSO₄·3H₂O
- Mohs hardness
- 2
- Density
- 2.21 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Crystalline Crusts, Efflorescent Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Copper-bearing Sulfide Deposits
- Typical price
- $20-100 thumbnail
Where rockhounds find bonattite
Classic worldwide localities
- Tuscany, Italy
- Chuquicamata, Chile
- Rio Tinto, Spain
Field-hunting tip
Look in oxidized zones of copper-bearing sulfide deposits country — that is the host setting where bonattite typically forms. If you start seeing chalcanthite, gypsum, jarosite in float, you are in the right ground. Field specimens usually show a fibrous, crystalline crusts, efflorescent aggregates habit, so train your eye for that shape before scanning the outcrop.





