Eriochalcite is a rare, water-soluble copper chloride mineral often found as crusts or efflorescences in volcanic environments. It is highly sensitive to humidity and must be stored in a dry, sealed container to prevent it from deliquescing or altering.
Is this eriochalcite?
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 eriochalcite with a known reference. Eriochalcite 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. Eriochalcite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Eriochalcite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, blue-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crusts, efflorescences, stalactitic.
Often confused with
Eriochalcite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside eriochalcite
Minerals reported to co-occur with eriochalcite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuCl₂·2H₂O
- Mohs hardness
- 2.5
- Density
- 2.38 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Crusts, Efflorescences, Stalactitic
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Volcanic Fumaroles and Oxidized Copper Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find eriochalcite
Classic worldwide localities
- Vesuvius, Italy
- Chuquicamata, Chile
- Tsumeb, Namibia
Field-hunting tip
Look in volcanic fumaroles and oxidized copper deposits country — that is the host setting where eriochalcite typically forms. If you start seeing atacamite, tenorite, cuprite in float, you are in the right ground. Field specimens usually show a crusts, efflorescences, stalactitic habit, so train your eye for that shape before scanning the outcrop.




