Basalt
Historical document, translated for reference. It reflects medical knowledge of the 1920s–30s and is not medical advice.
Summary
Basalt is a dark, often black, basic extrusive igneous rock that is chemically and mineralogically identical to the intrusive rock gabbro. It is primarily used as a building material, especially for pavements, and for the facing of foundations and monuments.
Encyclopedia entry (1928–1936)
Basalt, dark, often black, basic extrusive igneous rock, chemically and mineralogically identical to the intrusive rock "gabbro". The main minerals of basalt: basic plagioclases, augite and often olivine. Distribution in the USSR: Caucasus, Transbaikal, Altai, Kamchatka. Basalt - dense, uniform, heavy rocks, occurring most often in the form of flows and sheets, in which this rock appears as characteristic columnar, separating from other rocks, breaking down into 5-6-sided columns. In the chemical composition of basalt, the low content of silica (up to 40%) is characteristic; Al2O3 - from 10 to 20%; high content of MgO and CaO; sometimes significant iron content - from 10 to 25% and a small amount of alkalis (Na2O > K2O). Basalt serves as a building material, is used, mainly, for pavements, as well as for the facing of foundations and construction of monuments.
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“Basalt.” Soviet Medical Encyclopedia. English translation of Bolshaya Meditsinskaya Entsiklopediya, 1st ed. (Moscow, 1928–1936), ed. N. A. Semashko. https://sovietmedicalencyclopedia.pages.dev/article/basalt/