
Andalusite
Aluminium silicate (Al2SiO5)
A pleochroic aluminum silicate that flashes green and reddish-brown from different angles, with a cross-marked variety called chiastolite.
- Mohs hardness
- 7-7.5
- Color
- Brown, green, pink, yellow; strongly pleochroic
- Type
- mineral
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Overview
Andalusite is an aluminum silicate (Al2SiO5) and one of three polymorphs sharing that formula, alongside kyanite and sillimanite. Each forms under different temperature and pressure conditions, making andalusite an important indicator mineral for geologists mapping metamorphic grade.
Its standout gemological feature is strong pleochroism: a single faceted stone displays green, yellow, and reddish-brown flashes depending on viewing angle, earning it the nickname 'poor man's alexandrite,' though the effect differs from true color change.
A distinctive variety, chiastolite, contains dark carbonaceous inclusions arranged in a cross pattern visible in cross-sections, long valued as a protective talisman.
Formation & geology
Andalusite forms during regional and contact metamorphism of aluminum-rich (pelitic) sedimentary rocks such as shales and mudstones, under relatively low pressure and moderate temperature. It is common in metamorphic aureoles surrounding igneous intrusions.
It occurs in schists, gneisses, and hornfels, and as detrital grains in placer deposits where the durable crystals accumulate after weathering. Chiastolite develops when carbon-rich impurities are pushed into a cross arrangement as the crystal grows.
Notable localities include Andalusia in Spain (the namesake), Brazil, Sri Lanka, and the United States. Massive industrial-grade andalusite is mined in South Africa and France.
How to identify it
Look for elongated, near-square prismatic crystals, often brown, pinkish, or olive-green. The hallmark test is pleochroism: rotate a transparent stone and watch for distinct green and reddish-brown colors from different directions, visible even to the naked eye.
Hardness is 7-7.5, luster vitreous, and streak white. Chiastolite shows a dark cross or checkerboard when sliced and polished perpendicular to the crystal length.
Look-alikes include tourmaline and smoky quartz, but neither matches andalusite's strong green/brown pleochroism. It can also resemble its polymorph sillimanite; crystal habit, occurrence, and optics distinguish them. Distinct from alexandrite, which changes color with light source rather than viewing angle.
Uses & significance
Gem-quality andalusite is faceted for collectors and jewelry, with lapidaries orienting cuts to maximize the multicolor pleochroic play. Chiastolite is carved into cabochons, beads, and amulets featuring the natural cross.
Industrially, andalusite is far more important than as a gem. When heated it converts to mullite, a highly refractory material, so it is a key raw ingredient for high-temperature refractory bricks and linings used in steel, glass, and cement furnaces.
Metaphysically, chiastolite has been worn for centuries as a protective and grounding stone, associated with balance during change, though such properties are not scientifically established.
Frequently asked questions
What is chiastolite?
Chiastolite is a variety of andalusite containing dark carbon inclusions arranged in a cross or X pattern, visible when the crystal is sliced across its length. It is also called cross stone.
Why does andalusite change color?
It does not truly change color. It is strongly pleochroic, meaning it shows different colors (green, yellow, reddish-brown) depending on the angle you view it from, not the light source.
Is andalusite related to kyanite?
Yes. Andalusite, kyanite, and sillimanite are polymorphs sharing the formula Al2SiO5, each forming under different temperature and pressure conditions.
Is andalusite durable enough for rings?
At 7-7.5 Mohs it is reasonably durable for jewelry, though protective settings are wise for daily-wear rings to guard against knocks.
Andalusite guides
In-depth guides for identifying, valuing, and understanding Andalusite.











