Rock Identifier
Polished obsidian (Volcanic glass; predominantly rhyolitic SiO₂) — igneous
igneous

Polished obsidian

Volcanic glass; predominantly rhyolitic SiO₂

AI-generated identification · may be incorrect

Typically black to dark gray with a vitreous luster, conchoidal fracture, and no visible crystals; Mohs hardness about 5–5.5 and specific gravity about 2.35–2.65. The specimen appears polished and may show gray flow banding or sheen.

Identified More igneous
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Physical properties

Typically black to dark gray with a vitreous luster, conchoidal fracture, and no visible crystals; Mohs hardness about 5–5.5 and specific gravity about 2.35–2.65. The specimen appears polished and may show gray flow banding or sheen.

Formation & geological history

Forms when silica-rich lava cools extremely rapidly, preventing crystallization; most examples are Quaternary to recent in age and occur around young volcanic fields.

Uses & applications

Used for ornamental objects, cabochons, beads, knives, arrowheads, and lapidary carvings; historically valued for exceptionally sharp cutting edges.

Geological facts

Obsidian is technically volcanic glass rather than a fully crystalline rock and can weather into perlite or devitrified material over time.

Field identification & locations

Identify by its glassy luster, sharp conchoidal edges, lack of crystals, and uniform dark color; common sources include Mexico, the western United States, Armenia, Iceland, and Japan. The pictured piece is consistent with polished dark obsidian, though a photo cannot exclude man-made glass.