Rock Identifier
Tumbled black stone, likely black obsidian (Obsidian — natural volcanic glass, predominantly silica-rich rhyolitic composition) — igneous
igneous

Tumbled black stone, likely black obsidian

Obsidian — natural volcanic glass, predominantly silica-rich rhyolitic composition

AI-generated identification · may be incorrect

Typically black, opaque, and vitreous to subdued glassy luster; hardness about 5–5.5 Mohs, no crystal structure or cleavage, conchoidal fracture, and specific gravity around 2.3–2.6. The rounded edges indicate tumbling or polishing.

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Physical properties

Typically black, opaque, and vitreous to subdued glassy luster; hardness about 5–5.5 Mohs, no crystal structure or cleavage, conchoidal fracture, and specific gravity around 2.3–2.6. The rounded edges indicate tumbling or polishing.

Formation & geological history

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

Uses & applications

Used for ornamental carvings, cabochons, beads, arrowheads, and decorative objects; historically fashioned into exceptionally sharp cutting tools. Small polished pieces generally have modest value.

Geological facts

Obsidian is technically volcanic glass rather than a fully crystalline mineral. Similar-looking black stones may include basalt, black jasper, tourmaline, or manufactured glass.

Field identification & locations

Look for uniform glassy black color, conchoidal fracture, sharp chips, and absence of visible grains; a scratch test and inspection for bubbles can help distinguish it from glass, though this image alone is not definitive. Commonly found near rhyolitic lava flows.