Rock Identifier
Polished blue-black cabochon, likely blue obsidian or dyed glass-like stone (Indeterminate from image; possible natural obsidian (volcanic glass), commonly SiO₂-rich rhyolitic glass) — gemstone
gemstone

Polished blue-black cabochon, likely blue obsidian or dyed glass-like stone

Indeterminate from image; possible natural obsidian (volcanic glass), commonly SiO₂-rich rhyolitic glass

AI-generated identification · may be incorrect

Highly polished, domed cabochon with deep cobalt-blue color, black margins, and vitreous luster. Obsidian has Mohs hardness about 5–5.5, no cleavage, amorphous structure, and specific gravity around 2.35–2.65; the intense uniform blue may indicate dyeing or synthetic material.

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Physical properties

Highly polished, domed cabochon with deep cobalt-blue color, black margins, and vitreous luster. Obsidian has Mohs hardness about 5–5.5, no cleavage, amorphous structure, and specific gravity around 2.35–2.65; the intense uniform blue may indicate dyeing or synthetic material.

Formation & geological history

Natural obsidian forms when silica-rich lava cools rapidly, generally during Quaternary to older volcanic activity. Blue varieties are uncommon; without testing, dyed chalcedony, synthetic glass, or another treated stone cannot be excluded.

Uses & applications

Used as a jewelry cabochon, ornamental stone, or collector piece; obsidian is also used for decorative objects and exceptionally sharp experimental tools.

Geological facts

Obsidian lacks true crystals because it cools too quickly for crystallization. A flashlight may reveal translucency at thin edges, while conchoidal fracture is characteristic of natural obsidian.

Field identification & locations

Inspect edges and inclusions with magnification; glassy bubbles, perfectly uniform color, or dye concentration suggest imitation or treatment. Common obsidian sources include Mexico, the western United States, Armenia, and Turkey.