Sort of. Granite is primarily composed of quartz and feldspar. Hornblende is often present, but it usually is not one of the main components.
Mainly Quartz, Feldspar, and Hornblende. Often there is Mica (usually biotite or muscovite). By the way, these are minerals, not rocks that make up granite. Granite IS the rock.
Mica, hornblende, feldspar, and quartz mixed together make up a rock known as granite. Granite is a common type of igneous rock that is typically found in the Earth's continental crust. It is known for its durability, strength, and attractive appearance, making it a popular choice for construction and decorative purposes.
The mineral assemblage of Rhyolite is usually quartz, alkali feldspar and plagioclase (in a ratio > 1:2) and biotiteand hornblende are common accessory minerals. More importantly quartz has got to comprise more than 69% of the rock.
No, granite is not magnetic and cannot be moved with a magnet. The minerals that make up granite, such as quartz and feldspar, are not attracted to magnets.
Quartz will probably be found in most igneous and metamorphic rocks. Granite is a classic example of a rock with quartz in it. Search for images of "granite." Quartz sandstone is another rock practically made entirely up of quartz.
granite
Granite is defined as a course grained rock that must have plagioclase feldspar, potassium (aka alkali) feldspar, and quartz. Granite can also have a number of secondary minerals like micas or hornblende, but these secondary minerals do not have to be present.
Quartz itself is the mineral. Its formula is SiO2. Rocks are aggregates of minerals, so an example of a rock that contains a lot of quartz is granite.
In the volcano/magma chamber, different minerals that make up granite, (feldspar, quartz, etc.) mix to form grainy, large crystals of the different minerals. That is how granite is formed.
The four minerals that make up rocks in the intermediate family are plagioclase feldspar, amphibole (such as hornblende), biotite, and quartz. These minerals are typically found in rocks like diorite and andesite, which have a composition between felsic and mafic rocks.
Rocks are composed of minerals.
The tiny quartz particles that make up beaches come from the erosion of rocks containing quartz, such as granite and sandstone. These rocks are weathered over time by wind, water, and waves, breaking down into smaller and smaller grains that eventually make up the sandy beaches we see.