Hydrocerussite is a secondary mineral typically found in the oxidation zones of lead ore deposits. It often forms as a thin, pearly white coating on other lead minerals like cerussite or galena, though well-formed hexagonal crystals are highly sought after by collectors.
Is this hydrocerussite?
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 hydrocerussite with a known reference. Hydrocerussite sits at Mohs 3.5, 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, pearly on {0001}.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy.
Often confused with
Hydrocerussite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hydrocerussite
Minerals reported to co-occur with hydrocerussite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃(CO₃)₂(OH)₂
- Mohs hardness
- 3.5
- Density
- 6.80-6.82 g/cm³
- Streak
- White
- Luster
- Adamantine, pearly on {0001}
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy
- Cleavage
- On {0001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in the oxidized portions of lead deposits
Where rockhounds find hydrocerussite
Classic worldwide localities
- Mammoth-St. Anthony mine, Tiger, Pinal Co., Arizona, USA
- C & B mine, Gila Co., Arizona, USA
- Bunker Hill mine, Shoshone Co., Idaho, USA
- Långban, Värmland, Sweden
- Tvedalen, near Larvik, Norway
- Relatively Higher Pitts Farm, Mendip Hills, and as Merehead quarry, near Shepton Mallet, Somerset, England
Field-hunting tip
Where it forms: An uncommon secondary mineral in the oxidized portions of lead deposits. If you start seeing lead, cerussite, leadhillite in float, you are in the right ground. Typical habit: platy. Train your eye for that shape before scanning the outcrop.







