Pumice

Dentistry, Chemistry & Physics

Also known as: Lapis Pumicis, Scoria

Historical document, translated for reference. It reflects medical knowledge of the 1920s–30s and is not medical advice.

Summary

This article from the 1928–1936 Soviet medical encyclopedia describes pumice as a volcanic mineral, detailing its chemical composition, formation from rapidly cooled lava, and its historical and practical uses in medicine, dentistry, and industry.

Encyclopedia article (1928–1936)

PUMICE (Pumex, Lapis Pumicis), a mineral of volcanic origin belonging to the rhyolite or liparite rock family. Rhyolites have a composition similar to granite: SiO2 — 72%, Al2O3 — 16%, FeO.Fe2O3 — 1.5%, CaO — 1.5%, MgO — 0.5%, K2O — 2.5%. A variety of rhyolite, consisting chemically of acidic volcanic glass and passing into a homogeneous light-colored and vesicular glassy rock, is called pumice. P. is formed during the rapid cooling of lava and the presence of a large amount of water vapor in it; in this case, the rapid release of vapor promotes the formation of a spongy, foamy mass consisting of intersecting thin glassy films. P. consists of light pieces of white, gray, and yellow color, easily turning into powder. P. enters into the composition (5–10%) of pumice soap for washing heavily soiled hands and for rough skin; in dentistry, P. is applied for cleaning teeth; the application of P. in tooth powder is harmful, since P. damages tooth enamel. In cosmetics, P. is used for the destruction of hair on the face by means of daily careful wiping of the skin with a piece of P. P. is also applied for polishing wood, bone, horn, metal, etc., and in chemistry for the absorption of gases. In recent times, P. is widely applied in construction, giving a building material with cement.

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Cite this page

“Pumice.” Soviet Medical Encyclopedia. English translation of Bolshaya Meditsinskaya Entsiklopediya, 1st ed. (Moscow, 1928–1936), ed. N. A. Semashko. https://sovietmedicalencyclopedia.pages.dev/article/pumice/