Barylite is a rare barium beryllium silicate known for its strong blue fluorescence under short-wave ultraviolet light. It is most frequently found in metamorphic skarns or alkaline intrusive complexes as tabular crystals or in massive form.
Is this barylite?
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 barylite with a known reference. Barylite sits at Mohs 6.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Barylite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Barylite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish, blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive, granular.
Often confused with
Barylite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside barylite
Minerals reported to co-occur with barylite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaBe₂Si₂O₇
- Mohs hardness
- 6.5
- Density
- 4.05-4.08 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Distinct On {100}
- Fluorescence
- Strong Blue Under SW UV
- Rarity
- Rare
- Uses
- Collector, Mineralogical Specimen
- Host rock
- Metamorphic Skarns and Alkaline Igneous Pegmatites
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find barylite
Classic worldwide localities
- Långban, Sweden
- Khibiny Massif, Russia
- Mont Saint-Hilaire, Canada
- Franklin, New Jersey, USA
Field-hunting tip
Look in metamorphic skarns and alkaline igneous pegmatites country — that is the host setting where barylite typically forms. If you start seeing willemite, hardystonite, franklinite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







