Lafossaite is an extremely rare ammonium-lead chloride mineral first discovered in the fumarolic deposits of the La Fossa crater on Vulcano. It typically appears as small, cubic crystals associated with other sublimation products in geothermal volcanic environments.
Is this lafossaite?
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 lafossaite with a known reference. Lafossaite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lafossaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lafossaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: subhedral to euhedral crystals.
Often confused with
Lafossaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lafossaite
Minerals reported to co-occur with lafossaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb(NH₄)Cl₃
- Mohs hardness
- 2.5
- Density
- 2.35 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Subhedral to Euhedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Volcanic Fumaroles
- Typical price
- $50-300 per specimen
Where rockhounds find lafossaite
Classic worldwide localities
- La Fossa crater, Vulcano, Aeolian Islands, Italy
Field-hunting tip
Look in volcanic fumaroles country — that is the host setting where lafossaite typically forms. If you start seeing sal ammoniac, anglesite, galena in float, you are in the right ground. Field specimens usually show a subhedral to euhedral crystals habit, so train your eye for that shape before scanning the outcrop.






