Granite is formed from the slow cooling of high silicate magma intrusions that have risen through the crust and formed large bulbous chambers of molten material called plutons.
What is granite formed from.
Much of it was intruded during the precambrian age.
Plutons can take.
Granite is an intrusive igneous rock which means it was formed in place during the cooling of molten rock generally the slower the molten rock cooled the larger it s mineral crystals with k feldspar megacrysts forming in special circumstances greater than 5cm.
Granite coarse or medium grained intrusive igneous rock that is rich in quartz and feldspar.
It is the most common plutonic rock of the earth s crust forming by the cooling of magma silicate melt at depth.
Learn more about the properties and uses of granite in this article.
How is granite formed.
It forms from the slow crystallization of magma below earth s surface.
This would allow granite to form without melting pushing or exploding upwards towards the surface.
Granite is a common type of granular and phaneritic felsic intrusive igneous rock.
What granite means.
The average granite density ranges from 2 65 to 2 75 g cm3 165 to 172 lb cu ft its compressive strength is usually above 200 mpa and its viscosity near stp is 3 6 1019 pa s.
There are several types of granite including i type igneous s type sedimentary m type mantle and a type anorogenic.
Students of granites classify them in three or four categories.
Granite is composed mainly of quartz and feldspar with minor amounts of mica amphiboles and other minerals this mineral composition usually gives granite a red pink gray or white color with dark mineral.
It is formed from hot molten magma its colour can be dark or light grey brown or even pink according to the proportions of its minerals.
What sets granite apart from other rocks.
It is the most abundant basement rock that underlies the relatively thin sedimentary veneer of the continents.
Outcrops of granite tend to form tors domes or bornhardts and rounded massifs.
In reference to the coarse grained structure of such a holocrystalline rock the word granite comes from the latin granum a grain.
The magma is forced between other layers of rock by the pressure under the earth s surface.
I type igneous granites appear to arise from the melting of preexisting igneous rocks s type sedimentary granites from melted sedimentary rocks or their metamorphic equivalents in both cases.
Granite is more common in continental crust than in oceanic crust and has a felsic composition.
The differences between these types of granites are very subtle and long debated.
Granites depending on their mineralogy can be predominantly white pink or gray in colour.
Granite is a kind of igneous rock found on earth but nowhere else in the solar system.