Leucophanite is a rare beryllium silicate mineral most often found as transparent to translucent tabular, greenish-yellow crystals. It is highly prized by collectors for its strong luminescence under ultraviolet light and its distinctive lamellar structure. It is most famously recovered from the rare-alkaline pegmatites of the Langesundsfjord district in Norway.
Is this leucophanite?
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 leucophanite with a known reference. Leucophanite sits at Mohs 3.5-4, 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.
- 4Match the color rangeCompare against the expected color range: white, greenish yellow, yellow, light green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular.
Often confused with
Leucophanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside leucophanite
Minerals reported to co-occur with leucophanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCaBeSi₂O₆F
- Mohs hardness
- 3.5-4
- Density
- 2.96 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular
- Cleavage
- {001}, perfect; {100}, {010}, and {201}, distinct
- Fluorescence
- Pink under SW and LW UV
- Rarity
- Rare
- Uses
- Collector, Specimen
- Host rock
- In pegmatites in augite syenite (Langesundsfjord, Norway); in albitization zones in pegmatites at the contact of alkalic massifs intruding Proterozoic carbonaceous quartz-sericite schists (Baikal massif, Russia)
Where rockhounds find leucophanite
Classic worldwide localities
- Låven, Arø, Stokkø, Norway
- Morje, Telemark, Norway
- Vevja and Saga quarries, Tvedalen, Norway
- Lovozero massif, Kola Peninsula, Russia
- Baikal massif, eastern Siberia, Russia
- Narssârssuk, Greenland
Field-hunting tip
Where it forms: In pegmatites in augite syenite (Langesundsfjord, Norway); in albitization zones in pegmatites at the contact of alkalic massifs intruding Proterozoic carbonaceous quartz-sericite schists (Baikal massif, Russia). If you start seeing albite, orthoclase, natrolite in float, you are in the right ground. Typical habit: tabular. Train your eye for that shape before scanning the outcrop.








