Rock Identifier
Tumbled black stone, likely black obsidian (Obsidian (volcanic glass; composition typically rhyolitic)) — igneous
igneous

Tumbled black stone, likely black obsidian

Obsidian (volcanic glass; composition typically rhyolitic)

AI-generated identification · may be incorrect

Appears glossy, opaque, and black with a smooth tumbled surface. Obsidian has no crystal structure or cleavage and is about 5–5.5 on the Mohs scale; the photo alone cannot confirm the identification.

Identified More igneous →
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Physical properties

Appears glossy, opaque, and black with a smooth tumbled surface. Obsidian has no crystal structure or cleavage and is about 5–5.5 on the Mohs scale; the photo alone cannot confirm the identification.

Formation & geological history

Forms when silica-rich lava cools rapidly, preventing crystals from growing; it is generally geologically young compared with many crystalline rocks.

Uses & applications

Used for decorative objects, beads, jewelry, and historically for exceptionally sharp cutting tools.

Geological facts

Obsidian breaks with a distinctive curved, shell-like fracture and can produce edges sharper than surgical steel, though those edges are brittle.

Field identification & locations

Common sources include volcanic regions such as Mexico, the western United States, Iceland, and Japan. A glassy sheen and conchoidal fractures on a broken surface support identification; the pictured piece is too polished for a definitive ID.