Fluoro-cannilloite is an exceptionally rare member of the amphibole supergroup characterized by its fluorine-dominant site. It typically occurs as prismatic crystals within contact-metamorphosed limestone deposits and requires advanced analytical methods for positive identification.
Is this fluoro-cannilloite?
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-cannilloite with a known reference. Fluoro-cannilloite 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-cannilloite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fluoro-cannilloite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, yellow-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Fluoro-cannilloite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fluoro-cannilloite
Minerals reported to co-occur with fluoro-cannilloite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCa₂(Mg₄Al)(AlSi₇O₂₂)F₂
- Mohs hardness
- 5-6
- Density
- 3.31 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- Perfect in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Limestones
- Typical price
- expensive to rare market collector pricing
Where rockhounds find fluoro-cannilloite
Classic worldwide localities
- Pargas, Finland
Field-hunting tip
Look in metamorphic limestones country — that is the host setting where fluoro-cannilloite typically forms. If you start seeing calcite, diopside, phlogopite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






