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rhyolite |
Also found in: Wikipedia, Hutchinson | 0.10 sec. |
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rhyolite, fine-grained light-colored acidic volcanic rock rock, aggregation of solid matter composed of one or more of the minerals forming the earth's crust. The scientific study of rocks is called petrology. Rocks are commonly divided, according to their origin, into three major classes—igneous, sedimentary, and ..... Click the link for more information. . Rhyolite is chemically the equivalent of granite, and is thus composed primarily of quartz and orthoclase feldspar with subordinate amounts of plagioclase feldspar, biotite mica, amphiboles, and pyroxenes. Rhyolite lava exhibits a typical banded structure produced by its flow pattern. Rhyolite lavas occur in continental and submarine volcanoes, especially island arcs, and in igneous dikes. Rhyolite lavas are typically highly viscous and are explosively ejected from volcanoes. Rhyolites were formed in profusion in the Yellowstone Park area and throughout the southwestern portion of the United States. rhyoliteIgneous rock that is the volcanic equivalent of granite, whose chemical composition is similar. Rhyolites are known from all parts of the Earth and from all geologic ages; they are found mostly on the continents or their immediate margins, but small quantities have been described from remote islands. rhyolite [′rīยทə‚līt] (petrology) A light-colored, aphanitic volcanic rock composed largely of alkali feldspar and free silica with minor amounts of mafic minerals; the extrusive equivalent of granite. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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A 600 metre long, well expsed section of this zone has several ryholite domes of between 100 and 200 metres in diameter bounded to the south by a major fault. A 600 metre long, well exposed section, of this zone has several ryholite domes of between 100 and 200 metres in diameter bounded to the south by a major fault. All three holes intersected interbedded units of massive grey aphyric ryholite and intermediate to felsic tuffaceous rocks and bottomed in K- |
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