A kyanite blade is a distinctive elongated, bladed crystal, usually blue. Kyanite is famous for its anisotropic hardness, being much softer along the length of the blade than across it, which collectors can verify with a careful scratch test.
Is this kyanite blade?
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 kyanite blade with a known reference. Kyanite Blade sits at Mohs 4.5-7, 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: blue, white, gray, green, black.
- 5Look at form & habitCrystal system: triclinic. Typical habit: bladed, fibrous, radiating.
Often confused with
Kyanite Blade vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kyanite blade
Minerals reported to co-occur with kyanite blade. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₂SiO₅
- Mohs hardness
- 4.5-7
- Density
- 3.53-3.65 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Bladed, fibrous, radiating
- Cleavage
- Perfect
- Rarity
- Common
- Uses
- Collector, Industrial, Lapidary
- Host rock
- metamorphic schists and gneisses
Where rockhounds find kyanite blade
1 mapped spotsClassic worldwide localities
- Switzerland
- Brazil
- USA (North Carolina)
- India
- Nepal
Field-hunting tip
Where it forms: metamorphic schists and gneisses. If you start seeing garnet, staurolite, quartz in float, you are in the right ground. Typical habit: bladed, fibrous, radiating. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Pennsylvania. Start trip planning there.










