Avogadrite is a rare potassium fluoroborate mineral primarily found as a sublimation product in volcanic fumaroles. It typically occurs as tiny, colorless to white tabular crystals or crusts, often associated with other rare volcanic halides.
Is this avogadrite?
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 avogadrite with a known reference. Avogadrite 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. Avogadrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Avogadrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, incrustations, granular aggregates.
Often confused with
Avogadrite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside avogadrite
Minerals reported to co-occur with avogadrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Cs)BF₄
- Mohs hardness
- 2.5
- Density
- 2.62 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Incrustations, Granular Aggregates
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumaroles in Volcanic Environments
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find avogadrite
Classic worldwide localities
- Mount Vesuvius, Italy
- Vulcano, Lipari Islands, Italy
- Kamchatka Peninsula, Russia
Field-hunting tip
Look in fumaroles in volcanic environments country — that is the host setting where avogadrite typically forms. If you start seeing malladrite, hieratite, sulphur in float, you are in the right ground. Field specimens usually show a tabular crystals, incrustations, granular aggregates habit, so train your eye for that shape before scanning the outcrop.


