Granite is an intrusive igneous rock which is very hard crystalline and is visibly homogeneous in texture and forms by melting of continental rocks.
The process of granite formation.
The decaying material releases a significant amount of heat which melts the rocks around it.
Granite is more common in continental crust than in oceanic crust and has a felsic composition.
Since the time required to form granite is rather long it is both a strong and valuable stone.
Granite crystallizes from silica rich magmas that are miles deep in earth s crust.
Each rock has a unique formation process.
Granite is formed by the solidification of magma under the earth s surface.
This is an extremely slow process.
Formation of granite is explained below.
Granite s formation inside the earth below what is known as the mantle layer is a layer of molten rock formed by radioactive elements that occur naturally as the ground breaks down and decays.
They are crystallized by felsic melts that are less dense than mafia rocks and therefore tend to ascend to the surface.
The rocks in the earth s crust continuously undergo changes in their composition which leads to formation of other rocks.
Granite is actually made up of several different minerals including feldspar and quartz.
Generally the slower the molten rock cooled the larger it s mineral crystals with k feldspar megacrysts forming in special circumstances greater than 5cm.
To form granite magma must first cool underground.