Rock Identifier
Pumice (Pumice, a highly vesicular volcanic glass composed mainly of rhyolitic to dacitic silicate material) — igneous
igneous

Pumice

Pumice, a highly vesicular volcanic glass composed mainly of rhyolitic to dacitic silicate material

AI-generated identification · may be incorrect

Pale gray with a dull to slightly glassy luster and abundant small pores; hardness is variable, roughly 5–6 Mohs for its glassy material. The pictured piece appears weathered, and its mineral proportions and density cannot be confirmed from the image.

Identified More igneous
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Physical properties

Pale gray with a dull to slightly glassy luster and abundant small pores; hardness is variable, roughly 5–6 Mohs for its glassy material. The pictured piece appears weathered, and its mineral proportions and density cannot be confirmed from the image.

Formation & geological history

Forms when gas-rich, silica-rich lava cools rapidly during explosive eruptions, trapping bubbles in volcanic glass. It can form at many geological ages and is commonly deposited near volcanic centers or carried offshore.

Uses & applications

Used as an abrasive, exfoliating stone, lightweight aggregate, and horticultural soil amendment; attractive pieces may be collected, but this specimen is not gem material.

Geological facts

Pumice may be so porous that it floats temporarily. The holes and irregular shape are consistent with vesicular volcanic rock, though image-only identification is uncertain.

Field identification & locations

Look for a lightweight, frothy texture with many cavities and sharp, glassy-looking edges; common sources include volcanic regions such as Italy, Iceland, Greece, and the western United States.