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. Abellaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Abellaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: trigonal. 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 on Abellaite and pearly on Hydrocerussite.

How to tell apart: Cerussite is the harder of the two (Mohs 3-3.5 vs. 2); luster reads vitreous on Abellaite and adamantine 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
- 4.21 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect On {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-bearing Ores
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find abellaite
Classic worldwide localities
- Mina Eureka, Castell-estaó, Spain
Field-hunting tip
Look in oxidized lead-bearing ores country — that is the host setting where abellaite typically forms. If you start seeing hydrocerussite, cerussite, malachite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.


