Leightonite is a rare copper sulfate mineral primarily found in the oxidized zones of arid copper mines in Chile. It typically forms pale yellow to colorless tabular crystals or crusts and is highly valued by specialized mineral collectors due to its restricted distribution.
Is this leightonite?
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 leightonite with a known reference. Leightonite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Leightonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Leightonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pale yellow, white, colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts, granular aggregates.
Often confused with
Leightonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside leightonite
Minerals reported to co-occur with leightonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Ca₂Cu(SO₄)₄·2H₂O
- Mohs hardness
- 3
- Density
- 2.98 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Crusts, Granular Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Oxidized Copper Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find leightonite
Classic worldwide localities
- Chuquicamata Mine, Chile
- Potrerillos, Chile
Field-hunting tip
Look in oxidized copper deposits country — that is the host setting where leightonite typically forms. If you start seeing chalcanthite, kröhnkite, gypsum in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, granular aggregates habit, so train your eye for that shape before scanning the outcrop.




