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

Pumice

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

AI-generated identification · may be incorrect

Very lightweight, pale pink-tan, frothy and porous with a dull to silky luster; hardness about 5–6 Mohs, no cleavage, amorphous glassy structure, and typically low specific gravity (often floats).

Identified More igneous
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Physical properties

Very lightweight, pale pink-tan, frothy and porous with a dull to silky luster; hardness about 5–6 Mohs, no cleavage, amorphous glassy structure, and typically low specific gravity (often floats).

Formation & geological history

Forms when gas-rich felsic lava erupts explosively and rapidly cools, trapping abundant bubbles; specimens are generally geologically young, from Cenozoic to recent volcanic eruptions.

Uses & applications

Used as an abrasive, exfoliant, lightweight aggregate, soil additive, filtration medium, and decorative stone; usually low jewelry value.

Geological facts

Its holes are vesicles formed by expanding volcanic gases, and pumice can be transported long distances by water because it may float.

Field identification & locations

Identify it by its unusually low density, abundant interconnected pores, rough texture, and ability to scratch softer materials; common sources include Italy, Greece, Turkey, Iceland, the western United States, and New Zealand.