Bearsite is a rare beryllium arsenate mineral typically found as small, colorless to white tabular crystals or radiating aggregates. It is most famously associated with the phosphate-rich pegmatites of Hagendorf, Germany, where it occurs as a secondary mineral in late-stage hydrothermal vugs.
Is this bearsite?
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 bearsite with a known reference. Bearsite sits at Mohs 3, 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.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: encrustations, fibrous, striated.
Often confused with
Bearsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bearsite
Minerals reported to co-occur with bearsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Be₂(AsO₄)(OH)·4H₂O
- Mohs hardness
- 3
- Density
- 1.8-2 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Encrustations, fibrous, striated
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As a secondary mineral formed during the oxidation of an arsenic-bearing metal sulfide deposit associated with a felsite porphyry containing beryl
Where rockhounds find bearsite
Classic worldwide localities
- Found in the Bota-Burum uranium deposit, 15 km south of Alakol’ Lake, Chu-Ili Mountains, Kazakhstan
Field-hunting tip
Where it forms: As a secondary mineral formed during the oxidation of an arsenic-bearing metal sulfide deposit associated with a felsite porphyry containing beryl. If you start seeing pharmacosiderite, arseniosiderite, scorodite–mansfieldite in float, you are in the right ground. Typical habit: encrustations, fibrous, striated. Train your eye for that shape before scanning the outcrop.








