Rhyolite
This page is about a volcanic rock. For the satellite system, see Rhyolite/Aquacade.
Rhyolite is an
igneous, volcanic rock, of felsic composition . It may have any texture from aphanitic to
porphyritic. The
mineral assemblage is usually
quartz, alkali
feldspar and
plagioclase .
Biotite and
pyroxene are common accessory minerals.
Rhyolite can be considered as the extrusive equivalent to the
plutonic granite rock. Due to their high content of silica and low iron and magnesium contents, rhyolites polymerize quickly and form highly viscous
lavas.
Encyclopedia
This page is about a volcanic rock. For the satellite system, see Rhyolite/Aquacade.Rhyolite is an
igneous, volcanic rock, of felsic composition . It may have any texture from aphanitic to
porphyritic. The
mineral assemblage is usually
quartz, alkali
feldspar and
plagioclase .
Biotite and
pyroxene are common accessory minerals.
Rhyolite can be considered as the extrusive equivalent to the
plutonic granite rock. Due to their high content of silica and low iron and magnesium contents, rhyolites polymerize quickly and form highly viscous
lavas. They can also occur as
breccias or in
volcanic necks and dikes. Rhyolites that cool too quickly to grow crystals form a natural glass or vitrophyre, also called
obsidian. Slower cooling forms microscopic crystals in the lava and results in textures such as flow foliations, spherulitic, nodular, and lithophysal structures.
See also
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