Feldspathoid minerals · Reference guide

Sodalite

Often blue with pale patches, sodalite makes a useful comparison with lapis lazuli.

General mineral information, separate from our 17 photographed collection specimens.

Composition
Na₈Al₆Si₆O₂₄Cl₂
Mohs hardness
5.5–6
Read the clues
Appearance can vary
Dark blue sodalite-bearing rock crossed by pale veins on a turquoise background
Reference specimen · not from our collection

The source identifies this as a sodalite-bearing rock from Brazil. Notice how pale material divides the blue areas; the photograph does not identify every component.

Eurico Zimbres / CC BY-SA 2.5 (via Wikimedia Commons). Original image; displayed at a smaller size.

Identification clues

Blue is familiar, but sodalite also occurs in other colours. It is usually found in masses or grains rather than neat individual crystals. Surfaces can have a glassy to greasy-looking shine. In a mixed rock, describe each coloured area separately.

Mineral facts and formation

Sodalite belongs to the feldspathoid minerals and occurs in rocks such as nepheline syenite and phonolite. A specimen can contain sodalite alongside other minerals, so the whole piece need not share one composition or hardness.

Lookalikes and useful comparisons

Sodalite is a mineral species; lapis lazuli is a rock made from several minerals. Both can look blue and white. Gold-coloured flecks, their absence or the shade of blue cannot settle an identification on their own.

Care for a display specimen

Protect it from knocks and harder stones. For an unfamiliar display specimen, begin with a soft dry cloth on sound surfaces. Ask about dyes, coatings or repairs before trying cleaning products, and avoid aggressive scrubbing.

Read the full crystal care guide →

Look a little closer

Try this observation.

Sketch the outline of the blue areas in the reference photograph. Mark where pale material interrupts them. Your sketch should describe what is visible without naming every component.

Is every blue-and-white stone sodalite?

No. Colour combinations overlap between minerals, rocks and treated materials. A photograph is a starting point for observations; a reliable label or further examination is needed to identify an unknown specimen.

Sources and further reading

Reference information checked 4 October 2026. These sources describe minerals generally; they do not identify a particular stone.

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