Rock Identifier
Polished black obsidian (Volcanic glass, predominantly rhyolitic silica (SiO₂)) — igneous
igneous

Polished black obsidian

Volcanic glass, predominantly rhyolitic silica (SiO₂)

AI-generated identification · may be incorrect

Typically black, vitreous, and noncrystalline, with conchoidal fracture; Mohs hardness about 5–5.5 and specific gravity 2.35–2.65. The rounded, glossy piece appears polished or tumbled, though surface reflections obscure diagnostic detail.

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Physical properties

Typically black, vitreous, and noncrystalline, with conchoidal fracture; Mohs hardness about 5–5.5 and specific gravity 2.35–2.65. The rounded, glossy piece appears polished or tumbled, though surface reflections obscure diagnostic detail.

Formation & geological history

Forms when silica-rich lava cools so rapidly that crystals cannot grow, commonly during Quaternary volcanic eruptions. Major sources include the western United States, Mexico, Armenia, Iceland, Italy, and Japan.

Uses & applications

Used for ornaments, cabochons, beads, carvings, and decorative objects; historically fashioned into exceptionally sharp blades and arrowheads.

Geological facts

Obsidian is technically a mineraloid rather than a true mineral because it lacks an ordered crystal lattice. Flow bands, snowflake patterns, or translucent edges can indicate varieties or inclusions.

Field identification & locations

Identify by its uniform glassy luster, very smooth conchoidal fracture, lack of visible grains, and sharp edges when freshly broken; rule out black glass or slag, which may show bubbles or manufacturing textures.