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, 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.







