Pumice Pumice Paul B. Johnson, Jr. Category="Igneous rocks"Category="Volcanology"[image] 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. Pumice comes in many different colors such as white, yellowish, gray, gray brown, and a dull red.

It is widely used to make lightweight Concrete and as an Abrasive, especially in polishes and Cosmetics 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.