Penfieldite is a rare lead chloride mineral that typically forms as white, adamantine, hexagonal prismatic crystals. It is most famously associated with the ancient slag piles of Laurium, Greece, where it forms through the slow chemical alteration of lead-rich slag by seawater.
Is this penfieldite?
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 penfieldite with a known reference. Penfieldite sits at Mohs 3-4, 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 to greasy.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish, bluish.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: pyramidal, tabular.
Often confused with
Penfieldite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside penfieldite
Minerals reported to co-occur with penfieldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Cl₃(OH)
- Mohs hardness
- 3-4
- Density
- 5.82-6.61 g/cm³
- Streak
- White
- Luster
- Adamantine to greasy
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Pyramidal, tabular
- Cleavage
- {0001}, distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An alteration product of lead-bearing slag immersed in seawater (Laurium, Greece; Baratti Beach, Italy); in an oxidized hydrothermal lead deposit (Sierra Gorda district, Chile)
Where rockhounds find penfieldite
Classic worldwide localities
- Laurium, Greece, in slag
- Baratti Beach, Tuscany, Italy, in slag
- Margarita mine, Sierra Gorda district, southwest of Calama, Antofagasta, Chile
Field-hunting tip
Where it forms: An alteration product of lead-bearing slag immersed in seawater (Laurium, Greece; Baratti Beach, Italy); in an oxidized hydrothermal lead deposit (Sierra Gorda district, Chile). If you start seeing paralaurionite, phosgenite, fiedlerite in float, you are in the right ground. Typical habit: pyramidal, tabular. Train your eye for that shape before scanning the outcrop.





