Rock Identifier
Pumice (Pumice, vesicular volcanic glass, commonly rhyolitic to dacitic in composition) — igneous
igneous

Pumice

Pumice, vesicular volcanic glass, commonly rhyolitic to dacitic in composition

AI-generated identification · may be incorrect

Light gray, highly vesicular, dull to slightly glassy; typically Mohs 5–6, with no distinct cleavage and irregular fracture. The rounded shape may result from weathering or handling.

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Physical properties

Light gray, highly vesicular, dull to slightly glassy; typically Mohs 5–6, with no distinct cleavage and irregular fracture. The rounded shape may result from weathering or handling.

Formation & geological history

Forms when gas-rich, silica-rich lava rapidly cools and traps bubbles during explosive eruptions; it can be geologically recent or much older. The image alone cannot establish its age or exact composition.

Uses & applications

Used as an abrasive, lightweight aggregate, soil amendment, and in polishing and personal-care products; attractive pieces are collected.

Geological facts

Pumice is so porous that many pieces float initially, though they eventually become waterlogged.

Field identification & locations

Identify it by its abundant cavities and unusually low density; common deposits occur near volcanoes, including in Italy, Iceland, Turkey, and the western United States. Similar-looking vesicular rocks can be denser scoria.