Rhyolite, below that is pumice and in lower right corner is rhyolite (light color)]]Rhyolite can be considered as the extrusive equivalent to the plutonic granite rock. Due to their high content of silica, rhyolite form highly viscous lavas. They can also occur as breccias or in volcanic necks and dikes. Like obsidian, rhyolites frequently show flow, spherulitic, nodular, and lithophysal structures. See also: igneous rocks, list of rocks, granite
|
|
|
Home Alphabetical Listing Quote This article is from Wikipedia. All text is available under the terms of the GNU Free Documentation License. |