Fluorvesuvianite is a rare fluorine-dominant member of the vesuvianite group. It typically appears as colorlessish prismatic crystals in metasomatized carbonate rocks and is often difficult to distinguish from common vesuvianite without analytical testing.
Is this fluorvesuvianite?
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 fluorvesuvianite with a known reference. Fluorvesuvianite sits at Mohs 6, 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 silky.
- 4Match the color rangeCompare against the expected color range: colorless, silky white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: acicular, radial.
Often confused with
Fluorvesuvianite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fluorvesuvianite
Minerals reported to co-occur with fluorvesuvianite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₁₉Al(Al₁₀Mg₂)(SiO₄)₁₀(Si₂O₇)₄OF₉
- Mohs hardness
- 6
- Density
- 3.46 g/cm³
- Colors
- ColorlessSilky white
- Streak
- White
- Luster
- Vitreous silky
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Acicular, radial
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In coarse grained, chloritized diopside skarn
Where rockhounds find fluorvesuvianite
Classic worldwide localities
- Lupikko mine, Pitkäranta ore field, on the northeastern coast of Ladoga Lake, Karelia, Russia
Field-hunting tip
Where it forms: In coarse grained, chloritized diopside skarn. If you start seeing vesuvianite, clinochlore, sphalerite in float, you are in the right ground. Typical habit: acicular, radial. Train your eye for that shape before scanning the outcrop.






