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Volcanoes
Vicki M. Harder |
IntroductionA volcano is a vent through which magma, solid rock debris, and gases are erupted. The compositions of magma have a significant influence on the style and explosiveness of volcanic eruptions. The most common types of magma are basaltic, andesitic, and rhyolitic. Basaltic magma accounts for about 80 percent of all magma erupted by volcanoes. Whereas rhyolitic and andesitic magma accounts for 10 percent each.
Magma Characteristics and Volcanic LandformsThe viscosity, or the ability to flow, of a magma is dependent upon its temperature and silica and dissolved gas content. Basaltic magmas are the least viscous and rhyolitic magmas the most viscous. A volcanic landforms' shape is determined by the composition and characteristics of the volcanic materials and the types of eruptions that have occurred. Shield volcanoes are formed from the build-up of basaltic lava, forming a broad formation that resembles a shield lying horizontally, with an average slope of only a few degrees. Stratovolcanoes, also know as composite volcanoes, are built up of interlayers of andesitic lava and pyroclastic deposits, with very steep slopes. |
Eruptive StylesDissolved gases come out of solution during the upward movement of magma, forming bubbles. The ease or difficulty of the escape of the bubbles (magma viscosity) determines the eruptive style and explosiveness of a volcano. The melting temperature of a basaltic magma is approximately 1400 degrees C with a silica content in the 50 percent range, giving it a relatively low viscosity. The combination of high temperature and low viscosity allows the dissolved gas bubbles to escapee easily, creating a rather nonexplosive volcanic eruption. Temperature decreases and the silica content rises with andesitic and rhyolitic magmas with a corresponding increase in magma viscosity causing explosive eruptions. |
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Once you are at the Electronic Volcano Web site scroll down the screen until you come to "Catalogs".
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