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 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: green, brown, colorless, greenish yellow, yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive, prismatic.
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,Fe,Al,□)₁₀(Si,Al,B)₅O₂₁(OH,F)₂
- Mohs hardness
- 6-7
- Density
- 3.29-3.35 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent and opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, prismatic
- Cleavage
- Good on {110}
- Rarity
- Rare
- Uses
- Gemstone, Collector
- Host rock
- In boron-rich volcanic and sedimentary rocks subjected to amphibolite to granulite facies metamorphism; in metamorphosed anorthosite complexes
Where rockhounds find kornerupine
Classic worldwide localities
- Fiskenæsset, Greenland
- Bjordam, near Kragerö, Norway
- Waldheim, Saxony, Germany
- Mautia Hill, Tanzania
- Bok se Puts Farm, Namaqualand, Cape Province, South Africa
- Itrongahy, near Betroka, Madagascar
Field-hunting tip
Where it forms: In boron-rich volcanic and sedimentary rocks subjected to amphibolite to granulite facies metamorphism; in metamorphosed anorthosite complexes. If you start seeing sapphirine, cordierite, spinel in float, you are in the right ground. Typical habit: massive, prismatic. Train your eye for that shape before scanning the outcrop.








