Georgiadesite is an extremely rare lead-arsenic oxychloride mineral found primarily in the historic slag heaps of Laurium, Greece. It is highly sought after by systematic mineral collectors due to its very limited locality and unusual chemistry. Specimens are typically found as tiny, clear to yellow tabular crystals growing on top of other lead-bearing minerals.
Is this georgiadesite?
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 georgiadesite with a known reference. Georgiadesite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Georgiadesite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Georgiadesite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, sometimes in aggregates.
Often confused with
Georgiadesite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside georgiadesite
Minerals reported to co-occur with georgiadesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₁₆(AsO₃)₄Cl₁₄O(OH)₂
- Mohs hardness
- 3
- Density
- 6.05 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Sometimes in Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Slag Dumps From Ancient Lead Mining
- Typical price
- $200-1000+ for rare micro specimens
Where rockhounds find georgiadesite
Classic worldwide localities
- Laurium, Greece
Field-hunting tip
Look in slag dumps from ancient lead mining country — that is the host setting where georgiadesite typically forms. If you start seeing laurionite, fiedlerite, penfieldite in float, you are in the right ground. Field specimens usually show a tabular crystals, sometimes in aggregates habit, so train your eye for that shape before scanning the outcrop.





