Liroconite is a highly sought-after secondary copper mineral, famous for its intense sky-blue to deep green color and distinctively flattened, wedge-shaped crystals. It is primarily found in the oxidized zones of copper-arsenic deposits, historically reaching its finest aesthetic development in the mines of Cornwall, England.
Is this liroconite?
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 liroconite with a known reference. Liroconite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue to pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: sky blue, light blue, green, verdigris green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: euhedral crystals, granular.
Often confused with
Liroconite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Streak differs, so Liroconite leaves pale blue to pale green, Clinoclase leaves bluish green.

How to tell apart: Streak differs, so Liroconite leaves pale blue to pale green, Aurichalcite leaves light blue; luster reads vitreous to resinous on Liroconite and silky to pearly on Aurichalcite.
Often found alongside liroconite
Minerals reported to co-occur with liroconite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂Al(AsO₄)(OH)₄·4H₂O
- Mohs hardness
- 2-2.5
- Density
- 2.94-3.01 g/cm³
- Colors
- Streak
- Pale blue to pale green
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Euhedral crystals, granular
- Cleavage
- On {110}, {011}, indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in the oxidized zone of some copper deposits
Where rockhounds find liroconite
Classic worldwide localities
- Sterling Hill, Ogdensburg, Sussex Co., New Jersey, and at Bisbee, Cochise Co., Arizona, USA
- Cornwall, Wheals Muttrell and Gorland, also Wheal Unity and the Ting Tang mine, near Gwennap, England
- Wheal Cock, St. Just, England
- Saxony, from Schwarzenberg, Germany
- Sadisdorf copper mine, near Schmiedeberg, Germany
- Altväter samt Eschig mine, near Sayda, Germany
Field-hunting tip
Where it forms: A rare secondary mineral in the oxidized zone of some copper deposits. If you start seeing olivenite, chalcophyllite, clinoclase in float, you are in the right ground. Typical habit: euhedral crystals, granular. Train your eye for that shape before scanning the outcrop.




