Mullite is a rare high-temperature mineral typically formed by the thermal decomposition of aluminosilicates in fused xenoliths. It usually presents as thin, needle-like acicular crystals or fibrous masses embedded in glass. It is most famously found in the Tertiary igneous rocks of the Isle of Mull, Scotland.
Is this mullite?
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 mullite with a known reference. Mullite 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. Mullite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mullite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, colorless, pink.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular crystals, prismatic, fibrous, massive.
Often confused with
Mullite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mullite
Minerals reported to co-occur with mullite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₄Si₂O₁₀
- Mohs hardness
- 6-7
- Density
- 3.1-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular Crystals, Prismatic, Fibrous, Massive
- Cleavage
- Distinct On {110}
- Rarity
- Uncommon
- Uses
- Industrial, Refractory Material, Collector
- Host rock
- Thermally Metamorphosed Argillaceous Rocks, Fused Xenoliths
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find mullite
Classic worldwide localities
- Mull, Scotland
- Andernach, Germany
- Hatzfeld, Germany
- Krakow, Poland
Field-hunting tip
Look in thermally metamorphosed argillaceous rocks, fused xenoliths country — that is the host setting where mullite typically forms. If you start seeing sillimanite, corundum, sanidine in float, you are in the right ground. Field specimens usually show a acicular crystals, prismatic, fibrous, massive habit, so train your eye for that shape before scanning the outcrop.






