Rock Identifier
Tumbled black stone, likely black obsidian (Obsidian — natural volcanic glass, primarily SiO₂) — igneous
igneous

Tumbled black stone, likely black obsidian

Obsidian — natural volcanic glass, primarily SiO₂

AI-generated identification · may be incorrect

Usually black, vitreous and highly glossy with no visible crystals; Mohs hardness about 5–5.5, conchoidal fracture, no cleavage, and specific gravity around 2.35–2.ಿರಿಯ5. The rounded shape indicates tumbling or polishing.

Identified More igneous
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Physical properties

Usually black, vitreous and highly glossy with no visible crystals; Mohs hardness about 5–5.5, conchoidal fracture, no cleavage, and specific gravity around 2.35–2.ಿರಿಯ5. The rounded shape indicates tumbling or polishing.

Formation & geological history

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

Uses & applications

Used for ornamental carvings, cabochons, beads, polished stones, and historically very sharp blades; it has limited construction use.

Geological facts

Obsidian is technically a mineraloid rather than a true mineral because it lacks a crystal lattice. The dark red-brown translucent areas may indicate mahogany obsidian or internal iron-rich zones.

Field identification & locations

Identify by its glassy luster, uniform dark color, light weight relative to metallic minerals, and curved shell-like fracture; distinguish it from black glass by natural flow bands, inclusions, or translucence at thin edges. Exact identification is uncertain from the photograph alone.