Fluoro-edenite is a rare member of the amphibole group characterized by its sodium and fluorine-rich chemistry. It typically occurs as elongated prismatic or fibrous crystals in altered skarn environments and is notable for its historical association with health hazards in volcanic areas like Sicily.
Is this fluoro-edenite?
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 fluoro-edenite with a known reference. Fluoro-edenite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Fluoro-edenite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fluoro-edenite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, pale green, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic, fibrous, or acicular.
Often confused with
Fluoro-edenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fluoro-edenite
Minerals reported to co-occur with fluoro-edenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂Mg₅(Si₇Al)O₂₂F₂
- Mohs hardness
- 5-6
- Density
- 3.0-3.2 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic, Fibrous, Or Acicular
- Cleavage
- Perfect Prismatic
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Skarns and Altered Volcanic Rocks
- Typical price
- $20-100 per specimen
Where rockhounds find fluoro-edenite
Classic worldwide localities
- Biancavilla, Sicily, Italy
- Franklin, New Jersey, USA
- Various skarn deposits
Field-hunting tip
Look in metamorphic skarns and altered volcanic rocks country — that is the host setting where fluoro-edenite typically forms. If you start seeing calcite, diopside, garnet in float, you are in the right ground. Field specimens usually show a prismatic, fibrous, or acicular habit, so train your eye for that shape before scanning the outcrop.






