Rock Identifier
Pumice (Pumice, a highly vesicular volcanic rock composed mainly of volcanic glass with variable feldspar and silica minerals) — igneous
igneous

Pumice

Pumice, a highly vesicular volcanic rock composed mainly of volcanic glass with variable feldspar and silica minerals

AI-generated identification · may be incorrect

Light tan, porous, and dull to silky; its cavities (vesicles) formed as gas escaped from cooling lava. Hardness varies, typically about 5–6 Mohs for the glassy material; crystal structure is largely amorphous.

Identified More igneous
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Physical properties

Light tan, porous, and dull to silky; its cavities (vesicles) formed as gas escaped from cooling lava. Hardness varies, typically about 5–6 Mohs for the glassy material; crystal structure is largely amorphous.

Formation & geological history

Forms when gas-rich, silica-rich lava cools and depressurizes rapidly during explosive eruptions. It is geologically young volcanic material, though the specimen’s age and exact source cannot be determined from the image.

Uses & applications

Used as an abrasive, lightweight aggregate, and soil amendment; finer or shaped material is also used for cosmetic exfoliation and polishing.

Geological facts

Pumice is so full of gas bubbles that many pieces can float temporarily on water.

Field identification & locations

Look for a very lightweight, frothy rock with abundant interconnected pores and sharp, glassy surfaces. Common around explosive volcanoes, including in Italy, Iceland, and the western United States.