Rock Identifier
Snowflake Obsidian (Volcanic glass with Phenocrysts (SiO2 with Cristobalite inclusions)) — igneous
igneous

Snowflake Obsidian

Volcanic glass with Phenocrysts (SiO2 with Cristobalite inclusions)

Hardness: 5-5.5 on Mohs scale; Color: Black with white or gray 'snowflake' patches; Luster: Vitreous (glassy); Crystal structure: Amorphous (glass) with spherulitic cristobalite; Cleavage: None (conchoidal fracture); Specific gravity: 2.3-2.6

Hardness
5-5
Color
Black with white or gray 'snowflake' patches
Luster
Vitreous (glassy)
Identified More igneous

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Physical properties

Hardness: 5-5.5 on Mohs scale; Color: Black with white or gray 'snowflake' patches; Luster: Vitreous (glassy); Crystal structure: Amorphous (glass) with spherulitic cristobalite; Cleavage: None (conchoidal fracture); Specific gravity: 2.3-2.6

Formation & geological history

Formed through the rapid cooling of felsic (silica-rich) lava. The 'snowflakes' are formed as the glass begins to devitrify, creating radiating clusters of white cristobalite crystals within the dark glass matrix.

Uses & applications

Used primarily in jewelry (beads, cabochons), ornamental carvings, and as a popular specimen for rock collectors and metaphysical practitioners.

Geological facts

While regular obsidian is purely glass, Snowflake Obsidian is unique because it shows the early stages of a process where glass turns back into crystal. It was historically used by indigenous cultures to craft sharp tools and arrowheads.

Field identification & locations

Identify by its distinct black base and white, blotchy 'flower-like' patterns. It is commonly found in volcanic regions of the Western United States (Utah, California), Mexico, and Iceland. For collectors, look for high contrast between the black and white areas.