Rock Identifier
Pumice (Vesicular volcanic rock, primarily silica-rich volcanic glass (commonly rhyolitic or dacitic)) — igneous
igneous

Pumice

Vesicular volcanic rock, primarily silica-rich volcanic glass (commonly rhyolitic or dacitic)

AI-generated identification · may be incorrect

Light tan, highly vesicular, rough, dull to slightly glassy surface; Mohs hardness about 5–6, no cleavage, and unusually low density—often floats in water. The cavities formed by trapped volcanic gas are the key diagnostic feature.

Identified More igneous
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Physical properties

Light tan, highly vesicular, rough, dull to slightly glassy surface; Mohs hardness about 5–6, no cleavage, and unusually low density—often floats in water. The cavities formed by trapped volcanic gas are the key diagnostic feature.

Formation & geological history

Forms when gas-rich lava erupts explosively and cools rapidly, preserving abundant bubbles; specimens may range from recent volcanic material to deposits millions of years old.

Uses & applications

Used as an abrasive, exfoliant, polishing medium, lightweight aggregate, horticultural amendment, and in concrete or landscaping.

Geological facts

Pumice is not a mineral but a natural volcanic glass. Its pores can make it buoyant, though waterlogged pieces may eventually sink.

Field identification & locations

Identify it by its low weight, frothy texture, sharp pores, and lack of organized crystals; common sources include Italy, Turkey, Greece, the western United States, and New Zealand.