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<small>''Specimen of highly porous pumice from ] volcano <br>on ], ]. Density of specimen <br>approx 0.25 ]/]. Scale in ]s.''</small></div> <small>''Specimen of highly porous pumice from ] volcano <br>on ], ]. Density of specimen <br>approx 0.25 ]/]. Scale in ]s.''</small></div>


It is considered a ] because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in ]. It is widely used to make lightweight ] and as an ], especially in polishes and ] exfoliants. It is considered a ] because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in ]. It is widely used to make lightweight ] and as an ], especially in polishes and ] exfoliants.

Revision as of 05:11, 31 July 2004

File:Different rocks at Panum Crater-750px.jpg
Top stone is obsidian, below that is pumice and in lower right hand color is rhyolite (light color).

Pumice is a light, porous type of pyroclastic igneous rock. It is formed during explosive volcanic eruptions when liquid lava is ejected into the air as a froth containing masses of gas bubbles. As the lava solidifies, the bubbles are frozen into the rock. Any type of igneous rock - andesite, basalt, dacite or rhyolite - can form pumice given suitable eruptive conditions.


Specimen of highly porous pumice from Teide volcano
on Tenerife, Canary Islands. Density of specimen
approx 0.25 g/cm. Scale in centimetres.

It is considered a glass because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in water. It is widely used to make lightweight concrete and as an abrasive, especially in polishes and cosmetic exfoliants.

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