Kornerupine is a rare borosilicate mineral that forms elongated, prismatic crystals in high-grade metamorphic rocks. Collectors prize it for its unique color range, especially the rare blue-green hues, and its strong pleochroism which can shift from yellow-brown to green.
Is this kornerupine?
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 kornerupine with a known reference. Kornerupine 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. Kornerupine leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kornerupine typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellowish-green, brown, blue, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, fibrous, massive.
Often confused with
Kornerupine vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kornerupine
Minerals reported to co-occur with kornerupine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Fe²⁺)₄(Al,Fe³⁺)₆(SiO₄,BO₄)₅(OH,O)₂
- Mohs hardness
- 6.5-7
- Density
- 3.27-3.48 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Fibrous, Massive
- Cleavage
- Distinct in One Direction
- Rarity
- Rare
- Uses
- Gemstone, Collector
- Host rock
- Metamorphic Rocks Rich in Aluminum and Magnesium, Such as Granulites
- Typical price
- $50-500 per carat for gem quality, $20-150 for specimens
Where rockhounds find kornerupine
Classic worldwide localities
- Sri Lanka
- Madagascar
- Tanzania
- Canada
- Myanmar
Field-hunting tip
Look in metamorphic rocks rich in aluminum and magnesium, such as granulites country, the host setting where kornerupine typically forms. If you start seeing sapphire, spinel, garnet in float, you are in the right ground. Field specimens usually show a prismatic crystals, fibrous, massive habit, so train your eye for that shape before scanning the outcrop.







