Rock Identifier
Tumbled sodalite (Sodalite, Na₈(Al₆Si₆O₂₄)Cl₂) — mineral
mineral

Tumbled sodalite

Sodalite, Na₈(Al₆Si₆O₂₄)Cl₂

AI-generated identification · may be incorrect

Typically royal to denim blue with white calcite veining; vitreous to greasy luster and massive rather than visibly crystalline. Mohs hardness 5.5–6; cubic crystal system, poor cleavage, specific gravity about 2.2–2.4.

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Physical properties

Typically royal to denim blue with white calcite veining; vitreous to greasy luster and massive rather than visibly crystalline. Mohs hardness 5.5–6; cubic crystal system, poor cleavage, specific gravity about 2.2–2.4.

Formation & geological history

A feldspathoid mineral formed in silica-poor, sodium-rich igneous rocks, especially nepheline syenite; most deposits are Precambrian, though sodalite occurs in younger intrusions too.

Uses & applications

Used as a decorative stone, beads, carvings, and inexpensive jewelry; also collected as a mineral specimen.

Geological facts

Sodalite is named for its sodium content and is often confused with lapis lazuli, but it generally lacks lapis’s gold-colored pyrite flecks.

Field identification & locations

The vivid blue color with irregular white calcite patches is characteristic; notable sources include Canada, Brazil, Namibia, and Russia. The polished, rounded surface indicates a tumbled specimen.