Laurionite is a rare lead halide mineral famously associated with the ancient slag heaps of Laurium, Greece. It typically forms as delicate, colorless to white prismatic crystals in oxidized lead environments, often appearing in association with other lead minerals like cerussite.
Is this laurionite?
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 laurionite with a known reference. Laurionite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine, pearly on {100}.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crystalline, prismatic.
Often confused with
Laurionite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside laurionite
Minerals reported to co-occur with laurionite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCl(OH)
- Mohs hardness
- 3-3.5
- Density
- 6.241 g/cm³
- Streak
- White
- Luster
- Adamantine, pearly on {100}
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Crystalline, prismatic
- Cleavage
- {101}, distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Produced by the action of saline water on lead-bearing slag
Where rockhounds find laurionite
Classic worldwide localities
- Minnamax Cu–Ni sulfide deposit, Duluth Gabbro complex, near Hibbing, St. Louis Co., Minnesota, USA
- Laurium, Greece
- Baratti Beach, Tuscany, Italy
- Juliushütte, Astfeld, Harz Mountains, Germany
- Argent Pb–Zn mines, about 100 km east of Johannesburg, Transvaal, South Africa
- Mineral deposits at: Wheal Rose, near Sithney, Cornwall, and the Wesley mine, near Higher Pitts, Somerset, England
Field-hunting tip
Where it forms: Produced by the action of saline water on lead-bearing slag. If you start seeing paralaurionite, penfieldite, fiedlerite in float, you are in the right ground. Typical habit: crystalline, prismatic. Train your eye for that shape before scanning the outcrop.






