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 — that is 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.




