Linarite is a striking deep-blue secondary mineral found in the oxidation zones of lead-copper deposits. It is best identified by its intense azure color and characteristic tabular or prismatic crystal habits often found associated with anglesite or cerussite.
Is this linarite?
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 linarite with a known reference. Linarite 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 subadamantine.
- 4Match the color rangeCompare against the expected color range: deep blue, azure blue, sky blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: encrustations, platy, prismatic.
Often confused with
Linarite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside linarite
Minerals reported to co-occur with linarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCuSO₄(OH)₂
- Mohs hardness
- 2.5
- Density
- 5.35 g/cm³
- Streak
- Pale blue
- Luster
- Vitreous to subadamantine
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Encrustations, platy, prismatic
- Cleavage
- On {100}, perfect; on {001}, interrupted
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in the oxidized zone of Pb–Cu deposits
Where rockhounds find linarite
1 mapped spotsClassic worldwide localities
- Mammoth-St. Anthony mine, Tiger, Pinal Co., and in the Grand Reef mine, Santa Teresa Mountains, Graham Co., Arizona, USA
- Blanchard and Mex-Tex mines, near Bingham, Hansonburg district, Socorro Co., New Mexico, USA
- Tintic district, Juab Co., Utah, USA
- Cerro Gordo, Inyo Co., and on the Blue Bell claims, near Baker, San Bernardino Co., California, USA
- Linares, Jaén Province, Spain
- Arenas and San Giovanni, Sardinia, Italy
Field-hunting tip
Where it forms: An uncommon secondary mineral in the oxidized zone of Pb–Cu deposits. If you start seeing brochantite, anglesite, caledonite in float, you are in the right ground. Typical habit: encrustations, platy, prismatic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Mexico. Start trip planning there.







