Dacite generally erupts at temperatures between 800° and 1000°C. It is one of the most common rock types associated with enormous Plinian-style eruptions. When relatively gas-poor dacite erupts onto the surface of a volcano, it typically forms thick rounded lava flow in the shape of a dome.
Even though it contains less silica than rhyolite, dacite can be even more viscous (resistant to flow) and just as dangerous as rhyolites. These characteristics are a result of the high crystal content of many dacites, within a relatively high-silica melt matrix. Dacite was erupted from Mount St. Helens 1980–86, Mount Pinatubo in 1991, and Mount Unzen 1991–1996.
The word dacite comes from Dacia, a Roman province found between the Danube River and Carpathian Mountains, where the rock was first described.
Related category GEOLOGY AND PLANETARY SCIENCE
Source: U.S. Geological Survey
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