Beryllonite is a rare beryllium phosphate mineral typically found as transparent to translucent crystals in granite pegmatites. It is prized by collectors for its luster and clarity, though it is quite fragile due to its perfect cleavage and sensitivity to mechanical stress.
Is this beryllonite?
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 beryllonite with a known reference. Beryllonite sits at Mohs 5.5-6, 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 to adamantine, may be pearly on {010}.
- 4Match the color rangeCompare against the expected color range: colorless, white, light yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic, tabular, or equant crystals.
Often confused with
Beryllonite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Topaz is the harder of the two (Mohs 8 vs. 5.5-6).

How to tell apart: Danburite is the harder of the two (Mohs 7-7.25 vs. 5.5-6).

How to tell apart: Quartz is the harder of the two (Mohs 7 vs. 5.5-6).
Often found alongside beryllonite
Minerals reported to co-occur with beryllonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaBePO₄
- Mohs hardness
- 5.5-6
- Density
- 2.77-2.84 g/cm³
- Streak
- White
- Luster
- Vitreous to adamantine, may be pearly on {010}
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic, tabular, or equant crystals
- Cleavage
- {010}, perfect; {100}, good, interrupted; {101}, indistinct; {001}, in traces
- Rarity
- Rare
- Uses
- Collector, Lapidary
- Host rock
- As a rare secondary mineral in granitic and alkalic pegmatites
Where rockhounds find beryllonite
Classic worldwide localities
- Found on Sugarloaf Mountain, near Stoneham, at the Dunton quarry and the Bell Pit, Newry, Oxford Co., Maine, USA
- Occurs at Mont Saint-Hilaire, Quebec, Canada
- Found at the Viitaniemi pegmatite, Eräjärvi, Finland
- Norrö pegmatite, on Rånö Island, Sweden
- Meldon aplite, Okehampton, Devonshire, England
- Paprock, Laghman Province, Afghanistan
Field-hunting tip
Where it forms: As a rare secondary mineral in granitic and alkalic pegmatites. If you start seeing herderite, triplite, beryl in float, you are in the right ground. Typical habit: prismatic, tabular, or equant crystals. Train your eye for that shape before scanning the outcrop.






