What Is Pumice Rock Geology and Uses

Pumice is a light-colored volcanic rock. Its extremely porous, with a foamy appearance. Crushing pumice rock into a powder produces a substance called pumicite or simply volcanic ash. Key Takeaways: Pumice Rock Pumice is an igneous rock that forms when magma suddenly depressurizes and cools.Essentially, pumice is a solid foam. It is light enough to float on water until it becomes waterlogged.Pumice occurs worldwide wherever explosive volcanic eruptions have occurred. Leading producers include Italy, Turkey, Russia, United States, and Greece.Uses of pumice include making stone-washed jeans, as an abrasive, to retain moisture in horticulture, for water filtration, and to manufacture cement. How Pumice Forms Pumice forms when super-heated, pressurized molten rock violently erupts from a volcano. Gases dissolved in magma (mainly water and carbon dioxide) form bubbles when pressure suddenly decreases, in much the same way carbon dioxide bubbles form upon opening a carbonated drink. The magma swiftly cools, producing a solid foam. While pumicite may be produced by crushing pumice, it also occurs naturally. Fine-grained pumicite forms when magma containing a high concentration of dissolved gases suddenly depressurizes and cools. Volcanic eruptions can form vast beds of pumice, like this stone field in Argentina. E.Hanazaki Photography / Getty Images Pumice Composition Pumice forms so quickly that its atoms often dont have time to organize into crystals. Sometimes there are crystals present in pumice, but most of the structure is amorphous, producing a volcanic glass called a mineraloid. Pumice consists of silicates and aluminates. The silicic and felsic matter may include rhyolite, dactite, andesite, phonolite, pantellerite, trachyte, and (less commonly) basalt. Properties While pumice occurs in a variety of colors, it is almost always pale. Colors include white, gray, blue, cream, green, and brown. The pores or vesicles in the rock take two forms. Some vesicles are roughly spherical, while others are tubular. Probably the most significant property of pumice is its low density. Pumice tends to be so light that it floats on water until its vesicles fill and it eventually sinks. Before it sinks, pumice can float for years, potentially forming huge floating islands. Pumice rafts from the 1883 eruption of Krakatoa drifted around 20 years. Pumice rafting disrupts shipping and is important in the dispersal of marine organisms to new locations. Pumice Uses Pumice occurs in everyday products and has many commercial uses. Pumice stones are used as personal skin exfoliants. Stone-washed jeans are made by washing the denim with pumice rocks. The Greeks and Romans rubbed the rocks on their skin to remove unwanted hair. Because the rocks retain water, they are valued in horticulture to grow cacti and succulents. Pumice stones are natural exfoliants. Achim Sass / Getty Images Ground pumice is used as an abrasive in toothpaste, polishes, and pencil erasers. Some types of chinchilla dust bath powder consists of pumice powder. The powder is also used to make cement, filter water, and contain chemical spills. Where to Find Pumice Any violent volcanic eruption may produce pumice, so it is found worldwide. It is mined in Italy, Turkey, Greece, Iran, Chile, Syria, Russia, and the United States. Italy and Turkey led production in 2011, mining 4 million tonnes and 3 million tonnes, respectively. Pumice Versus Scoria Scoria is a porous rock that is darker and denser than pumice. lrosebrugh / Getty Images Pumice and scoria are two similar, commonly-confused igneous rocks. Scoria or lava rock forms when dissolved gases in magma come out of solution, producing bubbles that are frozen in shape when the molten rock cools. Like pumice, scoria contains porous vesicles. However, the walls of the vesicles are thicker. Thus, scoria is darker in color (black, purplish red, dark brown) and more dense than water (sinks). Sources Bryan, S.E.; A. Cook; J.P. Evans; P.W. Colls; M.G. Wells; M.G. Lawrence; J.S. Jell; A. Greig; R. Leslie (2004). Pumice rafting and faunal dispersion during 2001–2002 in the Southwest Pacific: record of a dacitic submarine explosive eruption from Tonga. Earth and Planetary Science Letters. 227: 135–154. doi:10.1016/j.epsl.2004.08.009Jackson, J.A.; Mehl, J; Neuendorf, K. (2005). Glossary of Geology. American Geological Institute. Alexandria, Virginia. 800 pp. ISBN 0-922152-76-4.McPhie, J., Doyle, M.; Allen, R. (1993). Volcanic Textures: A guide to the interpretation of textures in volcanic rocks. Centre for Ore Deposit and Exploration Studies. University of Tasmania, Hobart, Tasmania. ISBN 9780859015226.Redfern, Simon. Underwater volcano creates huge floating islands of rock, disrupts shipping. Phys.org. Omicron Technology Ltd.Venezia, A.M.; Floriano, M.A.; Deganello, G.; Rossi, A. (July 1992). Structure of pumice: An XPS and 27Al MAS NMR study. Surface and Interface Anal ysis. 18 (7): 532–538. doi:10.1002/sia.740180713