Fluorcanasite is a rare potassium-sodium-calcium silicate mineral primarily found in alkaline pegmatites. It is best known to collectors for its intense, bright yellow fluorescence under short-wave ultraviolet light, which makes it a highly prized display specimen.
Is this fluorcanasite?
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 fluorcanasite with a known reference. Fluorcanasite 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. Fluorcanasite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fluorcanasite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pinkish, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to acicular crystals, fibrous aggregates.
Often confused with
Fluorcanasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fluorcanasite
Minerals reported to co-occur with fluorcanasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₃Na₄Ca₂Si₁₂O₃₀F₄
- Mohs hardness
- 5-6
- Density
- 2.47 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Acicular Crystals, Fibrous Aggregates
- Cleavage
- Perfect in One Direction
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Agpaitic Pegmatites and Alkaline Igneous Complexes
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find fluorcanasite
Classic worldwide localities
- Kola Peninsula, Russia
- Khibiny Massif, Russia
Field-hunting tip
Look in agpaitic pegmatites and alkaline igneous complexes country — that is the host setting where fluorcanasite typically forms. If you start seeing aegirine, nepheline, eudialyte in float, you are in the right ground. Field specimens usually show a prismatic to acicular crystals, fibrous aggregates habit, so train your eye for that shape before scanning the outcrop.





