Phosgenite is a rare lead chloride carbonate typically found as a secondary mineral in oxidized lead deposits. It is highly prized by collectors for its brilliant adamantine luster and distinct tetragonal prismatic crystal habit, which often fluoresce a characteristic bright yellow under UV light.
Is this phosgenite?
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 phosgenite with a known reference. Phosgenite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Phosgenite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Phosgenite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray, yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic crystals, tabular.
Often confused with
Phosgenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside phosgenite
Minerals reported to co-occur with phosgenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Cl₂CO₃
- Mohs hardness
- 2.5-3
- Density
- 6.1-6.3 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic Crystals, Tabular
- Cleavage
- Distinct On {110}
- Fluorescence
- Bright Yellow Under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead Deposits
- Typical price
- $50-500 thumbnail
Where rockhounds find phosgenite
Classic worldwide localities
- Cromford, England
- Monteponi, Sardinia
- Broken Hill, Australia
- Touissit, Morocco
Field-hunting tip
Look in oxidized lead deposits country, the host setting where phosgenite typically forms. If you start seeing cerussite, anglesite, galena 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.




