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. Laurionite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Laurionite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, often elongated or tabular.
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
- 6.24 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Often Elongated or Tabular
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-bearing Ore Deposits
- Typical price
- $50-500 thumbnail
Where rockhounds find laurionite
Classic worldwide localities
- Laurium, Greece
- Tsumeb, Namibia
- Tiger, Arizona, USA
- Matlock, England
Field-hunting tip
Look in oxidized lead-bearing ore deposits country — that is the host setting where laurionite typically forms. If you start seeing cerussite, anglesite, phosgenite in float, you are in the right ground. Field specimens usually show a prismatic crystals, often elongated or tabular habit, so train your eye for that shape before scanning the outcrop.





