Chenite is an extremely rare lead-copper sulfate mineral known for its striking bright green, transparent crystals. It is primarily found as a secondary mineral in oxidized zones of lead-copper mines, often appearing as small, sharp tabular crystals in association with other lead minerals like linarite.
Is this chenite?
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 chenite with a known reference. Chenite 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: pale blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: sky blue.
- 5Look at form & habitCrystal system: triclinic. Typical habit: microscopic crystals, prismatic.
Often confused with
Chenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chenite
Minerals reported to co-occur with chenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuPb₄(SO₄)₂(OH)₆
- Mohs hardness
- ~2.5
- Density
- 5.98 g/cm³
- Colors
- Streak
- Pale blue
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Microscopic crystals, prismatic
- Cleavage
- On {100}, good; traces of a second one on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of rare occurrence in the oxidized portions of some Pb–Cu sulfide deposits
Where rockhounds find chenite
Classic worldwide localities
- Susanna mine, Leadhills, Lanarkshire, Scotland
- Llechwedd Helyg mine, Tir-y-Mynach, Dyfed, Wales
- Driggith mine, Caldbeck Fells, Cumbria, England
- Virneberg mine, near Rheinbreitbach, Rhineland-Palatinate, and at Ramsbeck, North Rhine-Westphalia, Germany
Field-hunting tip
Where it forms: Of rare occurrence in the oxidized portions of some Pb–Cu sulfide deposits. If you start seeing caledonite, linarite, leadhillite in float, you are in the right ground. Typical habit: microscopic crystals, prismatic. Train your eye for that shape before scanning the outcrop.







