Carobbiite is a rare potassium fluoride mineral typically found as small, colorless crystals in volcanic environments or pegmatites. It is highly water-soluble and can be easily confused with halite or sylvite, though it is usually distinguished by its specific formation environment and chemical tests.
Is this carobbiite?
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 carobbiite with a known reference. Carobbiite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral, massive, granular.
Often confused with
Carobbiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside carobbiite
Minerals reported to co-occur with carobbiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KF
- Mohs hardness
- 2-2.5
- Density
- 2.524 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Cubic
- Crystal habit
- Octahedral, massive, granular
- Cleavage
- {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In stalactites in cavities in lava
Where rockhounds find carobbiite
Classic worldwide localities
- Vesuvius, Campania, Italy
Field-hunting tip
Where it forms: In stalactites in cavities in lava. If you start seeing halite, mercallite, hieratite in float, you are in the right ground. Typical habit: octahedral, massive, granular. Train your eye for that shape before scanning the outcrop.




