Felsic igneous rocks (the lightest in color) are comprised mostly of quartz and potassium feldspar. Intermediate igneous rocks (somewhat darker than felsic) are made up of some quartz and potassium feldspar, but mostly plagioclase feldspar.
magma
felsic
True
Yes
Granite.
fine grained extrusive rocks can contain Potassium and Plagioclase Feldspar, Quartz, Biotite, Amphibole, Pyroxene and Olivine. these are all the choices for every igneous rocks
Granite is an intrusive igneous rock (formed from the slow cooling of magma underground), the major component of the continental crust, coarse grained, and composed of quartz along with a variety of feldspar minerals and micas.
Hornblende diorite is a type of intrusive igneous rock. It is composed primarily of plagioclase feldspar, hornblende, and small amounts of other minerals. It has a medium to coarse-grained texture and is typically gray or greenish in color.
Granitic Composition
because the magma does not have as much time for crystals to form inside the igneous rock therefor it is a fine-grained rock
it it feldspar
it it feldspar
Gabbro.
The larger crystals or masses of larger crystals are called phenocrysts.
Diorite is a speckled, coarse-grained igneous rock that is mainly composed of plagioclase, feldspar and hornblende. It is irregularly shaped, with randomly-oriented mineral crystals that form an interlocking texture.
An andesyte is a class of fine-grained intermediate igneous rock, mostly containing plagioclase feldspar.
Coarse-grained igneous rocks are formed when magma cools slowly deep inside the Earth. Creating big crystals in them.
fine grained extrusive rocks can contain Potassium and Plagioclase Feldspar, Quartz, Biotite, Amphibole, Pyroxene and Olivine. these are all the choices for every igneous rocks
Granite is an intrusive igneous rock (formed from the slow cooling of magma underground), the major component of the continental crust, coarse grained, and composed of quartz along with a variety of feldspar minerals and micas.
Intrusive igneous rocks commonly have large mineral crystals.
Metamorphic, igneous, and sedimentary rock are all composed of crystals, which vary greatly in size.
They are rocks formed from lava at or near the surface. Basalt is a typical fine-grained extrusive igneous rock, composed of mineral crystals that require magnification to see. The fine-grained texture is due to rapid solidification of the lava which leaves little time for large mineral crystal formation.