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, 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.





