Pseudocotunnite is a rare lead potassium chloride mineral typically formed by volcanic sublimation. It is most frequently encountered as yellow to colorless acicular or fibrous crystals forming crusts in active or dormant volcanic fumaroles.
Is this pseudocotunnite?
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 pseudocotunnite with a known reference. Pseudocotunnite sits at Mohs 2-3, 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: dull.
- 4Match the color rangeCompare against the expected color range: yellow, colorless, green yellow, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, aggregates, platy.
Often confused with
Pseudocotunnite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pseudocotunnite
Minerals reported to co-occur with pseudocotunnite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂PbCl₄
- Mohs hardness
- 2-3
- Density
- 4.25 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, aggregates, platy
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In volcanic fumaroles
Where rockhounds find pseudocotunnite
Classic worldwide localities
- Vesuvius, Campania, Italy
Field-hunting tip
Where it forms: In volcanic fumaroles. If you start seeing tenorite, cotunnite in float, you are in the right ground. Typical habit: acicular, aggregates, platy. Train your eye for that shape before scanning the outcrop.



