The Volcanic Fine Grained Compositional Equivalent Of Granite

It is the fine grained compositional equivalent of diorite.

The volcanic fine grained compositional equivalent of granite. Gabbro is the fine grained equivalent to basalt. The rock that is the fine grained equivalent of granite is. Igneous rocks are classified according to their mineral content. This chart illustrates the generalized mineral composition of igneous rocks.

The countertops in your kitchen might be made of granite as this rock is. Granites and rhyolites compositionally equivalent to granite but of a fine grain size are composed mainly of orthoclase feldspar quartz plagioclase feldspar mica and amphibole. Gabbro is a major component of the lower oceanic crust. Mafic rocks are dominated by plagioclase and pyroxene even if you can t see them with the naked eye and smaller amounts of olivine.

It contains more than 68 weight of silica in composition and is granular and coarse grained in texture. One example of an aphanitic rock with felsic composition. The general physical appearance of a rock as observed in reflected light. Because mafic lava is more mobile it is less common than basalt.

Moh s scale is. Which rock is the fine grained equivalent of granite. Ultramafic rocks are dominated by olivine and or pyroxene. Peridotite never contains olivine.

The fine grained equivalent of granite. Mauna loa in hawaii is situated on a hot spot. The softest mineral on mr. Click the circle by an answer with the mouse then click on the submit button to get a response.

Intermediate rocks are roughly even mixtures of felsic minerals mainly plagioclase and mafic minerals mainly hornblende pyroxene. A vesicular rock also known as cinder. Its principal minerals are feldspars quartz and mica. You will be told if your answer is correct or not and will be given some comments.

Heaton professor of earth sciences university of south dakota. Therefore plutonic rocks have coarse grained crystals. Granite the equivalent of its extrusive volcanic rock type rhyolite is a very common type of intrusive igneous rock. Material consisting of rock glass ash and scoria ejected during violent volcanic eruptions.

Rhyolite lavas are the most common lavas seen at mid ocean ridges.