Rock Identifier
Obsidian (specifically Rainbow or Silver Sheen Obsidian) (Volcanic Glass (predominantly SiO2)) — Igneous
Igneous

Obsidian (specifically Rainbow or Silver Sheen Obsidian)

Volcanic Glass (predominantly SiO2)

Hardness: 5–5.5 Mohs scale; Color: Black with metallic silver or rainbow iridescence; Luster: Vitreous (glassy); Crystal Structure: Amorphous (non-crystalline); Specific Gravity: 2.35–2.6; Conchoidal fracture.

Hardness
5–5
Color
Black with metallic silver or rainbow iridescence
Luster
Vitreous (glassy)
Identified More igneous

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Physical properties

Hardness: 5–5.5 Mohs scale; Color: Black with metallic silver or rainbow iridescence; Luster: Vitreous (glassy); Crystal Structure: Amorphous (non-crystalline); Specific Gravity: 2.35–2.6; Conchoidal fracture.

Formation & geological history

Formed when extrusive felsic lava cools rapidly with minimal crystal growth. The 'sheen' or 'rainbow' effect is caused by microscopic inclusions of gas bubbles or minerals like magnetite or feldspar oriented along flow layers. Typically found in young volcanic regions (Cenozoic to Holocene).

Uses & applications

Used primarily in jewelry (beads, cabochons), ornamental carvings, and historically for sharp tools/scalpels due to its ability to hold an edge thinner than steel.

Geological facts

Because it is glass, obsidian is metastable and eventually 'devitrifies' into crystalline quartz; thus, it is rarely found in rocks older than the Cretaceous period. It was one of the most highly traded materials in prehistoric times for making arrowheads and mirrors.

Field identification & locations

Identify by its glass-like texture, conchoidal (shell-like) fractures at the drill holes, and the unique internal 'glow' when rotated under a strong light source. Commonly found in Iceland, Mexico, and the Western United States (Oregon/California).