Granite ˈ ɡ r æ n ɪ t is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture.
Chemical formula of minerals in granite.
Other minerals can give granite its great variety of colors and textures.
Quartz content can range from 10 60 while the feldspar content typically ranges from 65 95 and biotite content is around 10 15 in most granite.
Other common minerals include mica muscovite and biotite and hornblende see amphibole.
Granites can be predominantly white pink or gray in color depending on their mineralogy the word granite comes from the latin granum a grain in reference to the coarse grained structure of such a completely crystalline rock.
Granite is a plutonic igneous rock.
Granite is the typical type of plutonic rocks it consists of feldspar quartz a few dark colored mineral sand mica.
Granite because it is composed of various and different quantities of minerals does not have a specific formula.
However granite is composed mainly of the minerals potassium feldspar quartz.
The resulting granite will likely have been made primarily from quartz different feldspars and biotite however it can also have a variety of other minerals and oxides present.
These minerals make up more than 80 of the rock.
Strictly speaking granite is an.
Another alkali feldspar is anorthoclase whose formula is na k alsi3o8.
These other minerals include mica amphibole hornblende biotite and muscovite.