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 — that is 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.







