Paralaurionite is a rare secondary mineral typically formed through the alteration of lead ores by seawater or chloride-rich solutions. It is most famous from the ancient slag piles of Laurion, Greece, where it occurs as small, clear, tabular or prismatic crystals often associated with other rare lead chlorides.
Is this paralaurionite?
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 paralaurionite with a known reference. Paralaurionite 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. Paralaurionite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Paralaurionite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, tabular.
Often confused with
Paralaurionite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paralaurionite
Minerals reported to co-occur with paralaurionite. 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
- 2.5
- Density
- 6.08 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Tabular
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-bearing Ore Deposits
- Typical price
- $50-500 depending on specimen quality and matrix
Where rockhounds find paralaurionite
Classic worldwide localities
- Laurion, Greece
- Mamut Mine, Malaysia
- Kombat Mine, Namibia
Field-hunting tip
Look in oxidized lead-bearing ore deposits country — that is the host setting where paralaurionite typically forms. If you start seeing laurionite, cerussite, phosgenite in float, you are in the right ground. Field specimens usually show a prismatic crystals, tabular habit, so train your eye for that shape before scanning the outcrop.





