What Is Not A Characteristic Of Granite A Common Intrusive Igneous Rock

What is not a characteristic of granite a common intrusive igneous rock.

What is not a characteristic of granite a common intrusive igneous rock.

Intrusive or plutonic igneous rocks form when magma cools slowly below the earth s surface most intrusive rocks have large well formed crystals. Examples include granite gabbro diorite and dunite. What is not a characteristic of granite a common intrusive igneous rock. Granite is a light colored igneous rock with grains large enough to be visible with the unaided eye.

It is mostly made of feldspar and quartz. Learn more about the properties and uses of granite in this article. 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 has a glassy appearance.

It is mostly made of feldspar and quartz. It is generally of a light color. A pluton is an igneous intrusive rock body that has cooled in the crust. Slow cooling allows time for large crystals to form so intrusive igneous rocks have visible crystals.

Granite coarse or medium grained intrusive igneous rock that is rich in quartz and feldspar. It is generally of a light color. Granite is the most common intrusive igneous rock see figure 1 for an example. This is not a characteristic of granite a common intrusive igneous rock.

It forms from the slow crystallization of magma below earth s surface. It has a glassy appearance. It has a phaneritic texture. Granites can be predominantly white pink or gray in color depending on their mineralogy the word granite comes from the latin granum a grain in reference to the coarse grained structure of such a completely crystalline rock.

It is generally of a light color. Granite ˈ ɡ r æ n ɪ t is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. It is the most common plutonic rock of the earth s crust forming by the cooling of magma silicate melt at depth.