Chalcanthite is a striking, deep blue secondary mineral typically found in the oxidized zones of copper deposits. It is famous for forming vibrant, crust-like aggregates or delicate, needle-like crystals, though it is highly fragile and readily dissolves in water.
Is this chalcanthite?
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 chalcanthite with a known reference. Chalcanthite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: green, green blue, light blue, dark blue.
- 5Look at form & habitCrystal system: triclinic. Typical habit: encrustations, reniform, stalactitic.
Often confused with
Chalcanthite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Azurite is the harder of the two (Mohs 3.5-4 vs. 2.5); streak differs, so Chalcanthite leaves white, Azurite leaves pale blue.

How to tell apart: Turquoise is the harder of the two (Mohs 5-6 vs. 2.5).

How to tell apart: Antlerite is the harder of the two (Mohs 3.5 vs. 2.5); streak differs, so Chalcanthite leaves white, Antlerite leaves pale green.
Often found alongside chalcanthite
Minerals reported to co-occur with chalcanthite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuSO₄·5H₂O
- Mohs hardness
- 2.5
- Density
- 2.286 g/cm³
- Streak
- White
- Luster
- Vitreous to resinous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Encrustations, reniform, stalactitic
- Cleavage
- Perfect on {110}; interrupted on {110}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- A secondary mineral in the oxidized portions of copper sulfide deposits, commonly of post-mining formation; rarely as a fumarolic deposit
Where rockhounds find chalcanthite
1 mapped spotsClassic worldwide localities
- United Verde mine, Yavapai Co., and in the Clifton-Morenci district, Greenlee Co., Arizona, USA
- Blue Bird mine, Fierro-Hanover district, Grant Co., New Mexico, USA
- Bluestone mine, Yerington district, Lyon Co., Nevada, USA
- Butte, Silver Bow Co., Montana, USA
- Vesuvius, Campania, Italy
- Rammelsberg and Goslar, Harz Mountains, Germany
Field-hunting tip
Where it forms: A secondary mineral in the oxidized portions of copper sulfide deposits, commonly of post-mining formation; rarely as a fumarolic deposit. If you start seeing melanterite, fibroferrite, rhomboclase in float, you are in the right ground. Typical habit: encrustations, reniform, stalactitic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Nevada. Start trip planning there.





