Abellaite is a very rare supergene mineral first discovered in the Eureka mine in Spain. It typically forms as delicate, hexagonal, transparent white platy crystals in oxidized zones of lead-rich ore deposits.
Is this abellaite?
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 abellaite with a known reference. Abellaite sits at Mohs 2, 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: vitreous to nacreous.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, crusts.
Often confused with
Abellaite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Hydrocerussite is the harder of the two (Mohs 3.5 vs. 2); luster reads vitreous to nacreous on Abellaite and adamantine, pearly on {0001} on Hydrocerussite.

How to tell apart: Cerussite is the harder of the two (Mohs 3-3.5 vs. 2); luster reads vitreous to nacreous on Abellaite and adamantine, tending toward vitreous, resinous on Cerussite.
Often found alongside abellaite
Minerals reported to co-occur with abellaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaPb₂(OH)(CO₃)₂
- Mohs hardness
- 2
- Density
- 5.93 g/cm³
- Streak
- White
- Luster
- Vitreous to nacreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy crystals, crusts
- Cleavage
- N.d.; synthetic analog perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A post-mining, secondary mineral that forms sparse coatings from supergene enrichment of a “red-bed”, sediment-hosted U-V-Cu deposit
Where rockhounds find abellaite
Classic worldwide localities
- Eureka mine, Castell-estaó, Catalan Pyrenees, Lleida province, Spain
Field-hunting tip
Where it forms: A post-mining, secondary mineral that forms sparse coatings from supergene enrichment of a “red-bed”, sediment-hosted U-V-Cu deposit. If you start seeing hydrozincite, aragonite, gordaite in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.






