Berborite is a rare beryllium borate mineral typically found as small, thin, colorless platy crystals in alkaline pegmatite environments. Collectors should look for it in association with other beryllium-bearing minerals, often requiring microscopic examination for positive field identification due to its small crystal size.
Is this berborite?
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 berborite with a known reference. Berborite 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: colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, tabular, massive.
Often found alongside berborite
Minerals reported to co-occur with berborite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Be₂BO₃(OH)·H₂O
- Mohs hardness
- 3
- Density
- 2.03-2.06 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy crystals, tabular, massive
- Cleavage
- Perfect on {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In serpentinized dolostone associated with W–Sr–B–Be-bearing skarns (Pitkäranta district, Russia); in vugs with natrolite (Saga quarry, Norway)
Where rockhounds find berborite
Classic worldwide localities
- Luppikko deposit, Pitkäranta district, Lake Ladoga, Karelia, Russia
- Saga and Tuften larvikite quarries, Tvedalen, and at Brønnebukta, Siktesøya Island, Langesundsfjord, Norway
Field-hunting tip
Where it forms: In serpentinized dolostone associated with W–Sr–B–Be-bearing skarns (Pitkäranta district, Russia); in vugs with natrolite (Saga quarry, Norway). If you start seeing hambergite, schoenfliesite, helvite in float, you are in the right ground. Typical habit: platy crystals, tabular, massive. Train your eye for that shape before scanning the outcrop.






