Prismatine is a rare borosilicate mineral that is structurally related to kornerupine, often requiring advanced analytical techniques to distinguish between the two. Collectors usually find it as prismatic to acicular crystals in high-grade metamorphic rocks like granulites or boron-rich metamorphic deposits.
Is this prismatine?
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 prismatine with a known reference. Prismatine sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Prismatine leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Prismatine typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, brown, blue, yellow, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, massive, fibrous.
Often confused with
Prismatine vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside prismatine
Minerals reported to co-occur with prismatine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Fe²⁺,Al)₅(Al,Mg)₁₂(Si,B,Al)₅O₂₁(OH,F)
- Mohs hardness
- 6.5-7
- Density
- 3.3-3.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Massive, Fibrous
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector, Gemstone
- Host rock
- Metamorphic Rocks
- Typical price
- $50-500 per gram for gem quality
Where rockhounds find prismatine
Classic worldwide localities
- Madagascar
- Sri Lanka
- Greenland
- Kenya
- Canada
Field-hunting tip
Look in metamorphic rocks country, the host setting where prismatine typically forms. If you start seeing sillimanite, garnet, cordierite in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, fibrous habit, so train your eye for that shape before scanning the outcrop.







