Herbertsmithite is a rare copper zinc hydroxychloride that forms distinctive bright green rhombohedral crystals. It is highly sought after by collectors for its significance in quantum physics research as a candidate for a quantum spin liquid. It is typically found as a secondary mineral in oxidized zones of copper deposits.
Is this herbertsmithite?
4-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 herbertsmithite with a known reference. Herbertsmithite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: dark green, blue green.
- 4Look at form & habitCrystal system: trigonal. Typical habit: aggregates, rhombohedral crystals.
Often confused with
Herbertsmithite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Luster reads vitreous on Herbertsmithite and adamantine to vitreous on Atacamite.

How to tell apart: Luster reads vitreous on Herbertsmithite and adamantine to vitreous on Clinoatacamite.
Often found alongside herbertsmithite
Minerals reported to co-occur with herbertsmithite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃Zn(OH)₆Cl₂
- Mohs hardness
- 3-3.5
- Density
- 3.75-3.95 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Aggregates, rhombohedral crystals
- Cleavage
- Good {101̄1}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in the oxidation zone of polymetallic mineral deposits
Where rockhounds find herbertsmithite
Classic worldwide localities
- Mina Los Tres Presidentes, Sierra Gorda, Chile, Iran
- Kali Kafi and Chah Khouni mines, Anarak, Iran
Field-hunting tip
Where it forms: A secondary mineral in the oxidation zone of polymetallic mineral deposits. If you start seeing gypsum, opal, dioptase in float, you are in the right ground. Typical habit: aggregates, rhombohedral crystals. Train your eye for that shape before scanning the outcrop.






