Rock Identifier
Likely pumice or vesicular volcanic rock (Pumice; predominantly volcanic glass (silica-rich, commonly rhyolitic or dacitic)) — igneous
igneous

Likely pumice or vesicular volcanic rock

Pumice; predominantly volcanic glass (silica-rich, commonly rhyolitic or dacitic)

AI-generated identification · may be incorrect

Pale gray-white, porous, and dull to slightly glassy; hardness about 5–6 Mohs, with abundant vesicles and very low density. The specimen appears irregular and may float if sufficiently porous.

Identified More igneous
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Physical properties

Pale gray-white, porous, and dull to slightly glassy; hardness about 5–6 Mohs, with abundant vesicles and very low density. The specimen appears irregular and may float if sufficiently porous.

Formation & geological history

Forms when gas-rich explosive magma rapidly decompresses and quenches, trapping bubbles in volcanic glass; typically Quaternary to recent, though older deposits are widespread.

Uses & applications

Used as an abrasive, lightweight aggregate, concrete additive, horticultural soil amendment, and cosmetic exfoliant; attractive pieces may be collected but have modest value.

Geological facts

Pumice is not crystalline like most rocks; its vesicles record escaping volcanic gases. A closely related, darker and denser material could be scoria, but this specimen’s light color favors pumice.

Field identification & locations

Common around explosive volcanic regions, including Italy, Greece, Turkey, Japan, New Zealand, Mexico, and the western United States. Confirm by testing low density, porous texture, and lack of reaction to dilute acid.