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Andesite (pronounced /ˈændəsaɪt/) is an extrusive igneous, volcanic rock, of intermediate composition, with aphanitic to porphyritic texture. In a general sense, it is the intermediate type between basalt and dacite. The mineral assemblage is typically dominated by plagioclase plus pyroxene and/or hornblende. Magnetite, zircon, apatite, ilmenite, biotite, and garnet are common accessory minerals. Alkali feldspar may be present in minor amounts. The quartz-feldspar abundances in andesite and other volcanic rocks are illustrated in QAPF diagrams. Relative alkali and silica contents are illustrated in TAS diagrams. (Source wikipedia)
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Feldspar minerals comes in a variety of colors and chemical formulas. The most common pink feldspar is orthoclase.
They are all found in Granite
Orthoclase is a common mineral and a member of the potassium feldspar group. It is used in the manufacture of glass and ceramics. One type is the moonstone gemstone.
The Top 10 Rock-Forming MineralsSilicate Minerals:QuartzFeldspar Group:K-Feldspar (Orthoclase)PlagioclaseOlivinePyroxene Group:AugiteAmphibole Group:HornblendeMica Group:MuscoviteBiotiteGarnetNon-silicate minerals:Calcite
Magma solidifies into a combination of minerals that are collectively called igneous rock. Minerals common in igneous rock are potassium feldspar, plagioclase feldspar, muscovite and biotite mica, quartz, hornblende, olivine, and magnetite.
Biotite and muscovite micas, quartz, magnetite, olivine, amphiboles, and feldspars.
Feldspar
Feldspar
Feldspar
The mineralogy of basalt is characterized by a preponderance of calcic plagioclase feldspar and pyroxene. Olivine can also be a significant constituent.
Igneous Rocks have many different mineral compositions.---- * Felsic-High in silica,low density,light colored* Mafic-less silica than felsic,dark colored,higher density than felsic * Ultramafic-lowest content of silica
There are ten minerals that are so common that they make up 90% of the Earth's crust. These are quartz, orthoclase, plagioclase, muscovite, biotite, calcite, dolomite, halite, gypsum, and ferromagnesian minerals.