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Vesicular pumice is an extrusive igneous rock that consists of a foam of mineral matter (usually silica-rich and glassy) enclosing bubbles of gas (usually carbon dioxide). The mineral material itself is denser that water, but the bubbles make the rock overall less dense than water, and it will float. Pieces of pumice may often be found washed up on beaches.

Pumice is formed when magma of intermediate or felsic composition having a large proportion of dissolved gasses is simultaneously rapidly de-pressurised and rapidly cooled. The gasses exsolve like bubbles in warm and shaken soda-pop, and the mineral matter solidifies before the foam can collapse.

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