Pumice

Missing image
Teidepumice.jpg
Specimen of highly porous pumice from Teide volcano on Tenerife, Canary Islands. Density of specimen approx 0.25 g/cm³. Scale is in cm.

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. When larger amounts of gas are present, the result is a finer-grained variety of pumice known as pumicite.

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.


When used as an additive for cement, a fine-grained version of pumice called pozzolan is mixed with lime to form a light-weight, smooth, plaster-like concrete. This form of concrete was used as far back as Roman times.

Missing image
Chrysocolla_USA.jpg


 This article about a specific mineral, mineraloid, or type of rock is a stub. You can help Wikipedia by expanding it.

See also: Pumice, Abrasive, Ancient Rome, Andesite, Basalt, Canary Islands, Cement, Cm, Concrete