How to identify Sodalite
Na8(Al6Si6O24)Cl2
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Open the appTo correctly identify Sodalite (Na8(Al6Si6O24)Cl2), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Typically deep royal blue, but can also be gray, green, yellow, pink, or white. Often mottled with white streaks or patches of calcite.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous to greasy.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Massive, granular, or as disseminated grains within host rock. Crystals are rare but can be dodecahedral.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Cubic system, typically forming dodecahedra, but more commonly found as massive aggregates or disseminated grains.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Poor to distinct in three directions (dodecahedral), but often difficult to observe in massive material.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in silica-undersaturated igneous rocks (e.g., nepheline syenites, phonolites) and associated metasomatic rocks (e.g., fenites). It is an indicator mineral for alkaline igneous activity.
Key Facts
- Hardness
- 5.5-6 (Mohs scale)
- Specific Gravity
- 2.13-2.29 g/cm³
- Crystal System
- Cubic
- Color
- Deep royal blue (most common), also gray, green, yellow, pink, white
- Luster
- Vitreous to greasy
- Transparency
- Transparent to opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- Poor to distinct dodecahedral {110}
- Composition
- Sodium aluminum silicate with chlorine
Physical characteristics
- Crystal Habit: Massive, granular, disseminated grains; rarely as dodecahedral crystals
- Cleavage Type: Poor to distinct dodecahedral {110}
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Vitreous to greasy
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