Lehmannite is a distinct yellow variety of beryl that typically exhibits a vibrant, deep golden to honey-yellow coloration. Collectors identify it by its hexagonal prismatic habit and high clarity, frequently found in granitic pegmatite environments alongside quartz and feldspar.
Is this lehmannite?
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 lehmannite with a known reference. Lehmannite sits at Mohs 7.5-8 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lehmannite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lehmannite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, golden.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Lehmannite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lehmannite
Minerals reported to co-occur with lehmannite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Be₃Al₂Si₆O₁₈
- Mohs hardness
- 7.5-8
- Density
- 2.6-2.9 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- Imperfect Basal
- Rarity
- Rare
- Uses
- Collector, Gemstone
- Host rock
- Granite Pegmatites
- Typical price
- $50-500 per specimen
Where rockhounds find lehmannite
Classic worldwide localities
- Minas Gerais, Brazil
- Volodarsk-Volynskyi, Ukraine
Field-hunting tip
Look in granite pegmatites country — that is the host setting where lehmannite typically forms. If you start seeing quartz, feldspar, mica in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






