Euclase is a rare beryllium aluminum silicate known for its brilliant blue or colorless, highly lustrous crystals. Collectors specifically look for its distinct, chisel-like crystal terminations and its propensity to cleave along one plane, which makes it challenging for lapidary work.
Is this euclase?
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 euclase with a known reference. Euclase sits at Mohs 7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Euclase leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Euclase typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, blue, greenish-blue, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals with distinct striations, often chisel-shaped.
Often confused with
Euclase vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside euclase
Minerals reported to co-occur with euclase. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BeAlSiO₄(OH)
- Mohs hardness
- 7.5
- Density
- 3.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals with Distinct Striations, Often Chisel-shaped
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Gemstone, Collector
- Host rock
- Pegmatites and Hydrothermal Veins
- Typical price
- $100-500 per carat for facet-grade gems, higher for rare crystals
Where rockhounds find euclase
Classic worldwide localities
- Minas Gerais, Brazil
- Ouro Preto, Brazil
- Zagi Mountains, Pakistan
- Urals, Russia
- Colombian emerald mines
Field-hunting tip
Look in pegmatites and hydrothermal veins country — that is the host setting where euclase typically forms. If you start seeing beryl, topaz, quartz in float, you are in the right ground. Field specimens usually show a prismatic crystals with distinct striations, often chisel-shaped habit, so train your eye for that shape before scanning the outcrop.






