Fassinaite is an extremely rare lead thiosulfate mineral that typically occurs as small, tabular crystals. It is primarily found as an alteration product of galena in lead-rich oxidation zones. Due to its rarity and delicate nature, it is highly sought after by advanced systematic mineral collectors.
Is this fassinaite?
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 fassinaite with a known reference. Fassinaite 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. Fassinaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fassinaite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Fassinaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fassinaite
Minerals reported to co-occur with fassinaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂S₂O₃
- Mohs hardness
- 2
- Density
- 5.68 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find fassinaite
Classic worldwide localities
- Fassina quarry, Italy
- Laurion, Greece
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where fassinaite typically forms. If you start seeing galena, cerussite, anglesite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.



