Mineral field guide

How to identify kyanite

Kyanite is a bladed aluminum silicate mineral with strongly directional hardness, commonly blue to gray, that forms in aluminum-rich metamorphic rocks at elevated pressure.

mineralAluminum silicate · Al₂SiO₅

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Intergrown bladed kyanite crystals about five centimeters across from Boehl’s Butte, Idaho
Intergrown bladed kyanite crystals from IdahoPhoto: Shannon Heinle · CC0 1.0 · Wikimedia Commons
Classification

What is kyanite?

Kyanite is Al₂SiO₅, the same chemical composition as andalusite and sillimanite but with a different crystal structure stable under different pressure-temperature conditions.

Appearance

What does kyanite look like?

Crystals are typically elongated, flattened blades with parallel striations and vitreous to pearly luster. Blue color may be patchy or concentrated along the crystal center.

Kyanite also occurs gray, white, green, blackish, or colorless and may form radiating aggregates or embedded blades in schist, gneiss, and quartz-rich rock.

Field tests

Identification tests

Begin with observation and use the least destructive test first. Results can change with weathering, mixtures, coatings, and grain size. Review the step-by-step field-test methods before altering an unfamiliar specimen.

Directional hardness

About 4.5 to 5 parallel to length and 6.5 to 7 across the blade

The unusual hardness anisotropy is a major clue on expendable material.

Cleavage

Perfect in one direction and good in another

Blades split along flat surfaces and may be brittle.

Habit

Elongated flattened blades

Separates it from equant corundum and many blue minerals.

Streak

White

Expected but not diagnostic.

Comparison

Common lookalikes

Corundum

Uniformly much harder at Mohs 9 and lacks kyanite’s bladed cleavage habit.

Blue tourmaline

Harder and commonly forms deeply striated trigonal prisms with poor cleavage.

Sillimanite

Commonly fibrous or slender-prismatic and does not show the same extreme directional hardness.

Geologic origin

How does it form?

Kyanite forms during medium- to high-grade metamorphism of aluminum-rich sedimentary rocks, especially under relatively high pressure.

Its presence helps constrain metamorphic conditions when mineral assemblage and regional context are evaluated together.

Where it occurs

Geologic setting and occurrence

Kyanite occurs in metamorphic belts, commonly in mica schist, gneiss, quartzite, and high-pressure metamorphic rocks.

Color alone cannot establish kyanite, and directional hardness should not be tested on valuable crystals.

Human use

Uses and significance

Kyanite and related aluminum silicates are used in heat-resistant refractories, ceramics, kiln furniture, foundry products, and other high-temperature applications.

Safety and limits

Field notes

  • Test hardness in two directions only on expendable material.
  • Bladed crystals can split and form sharp edges.
  • Do not infer metamorphic pressure from one loose specimen without field context.

This guide supports preliminary field identification, not a laboratory determination, appraisal, hazard assessment, or statement of ownership or collecting permission. Verify land status and local rules before handling or collecting material.

Source basis

Authoritative sources

LithoMap wrote this guide in original language using the scientific concepts and physical-property standards supported by these sources.

Editorial review: September 17, 2026.