The cooling rate of the rock.
Phaneritic refers to igneous rock grain size,which is visible with the naked eye.
The individual grains (crystals) in quickly cooled magma are described as aphanitic--not visible without magnification.
Igneous rocks can be strong due to their interlocking grain textures
Small to medium grain size.
The rate at which the igneous rock cools controls grain size. Slower cooling results in larger crystals while faster cooling results in smaller crystals.
The cooling rate of the rock.
It depend what rock it is but extrusive rocks generally non-crystalline or have a grain size of less than 1 mm
Phaneritic refers to igneous rock grain size,which is visible with the naked eye.
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
It depends on if it is intrusive or extrusive. If it is an intrusive rock, it is formed when magma hardens under the earth and has a larger grain size. If it is an extrusive rock, it is formed when lava hardens on the earth's surface and has a smaller grain size.
Crystal size in igneous rocks is controlled by the rate of cooling whereby the slower the rate, the larger the size of crystal.
yes, it does. when a grain size in an igneous rock is small, it means that it was probably an extrusive rock, meaning it formed on land. but if the grain size is big, it means that the rock most likely formed underground, or it was intrusive. try remembering it like this- the larger the crystals, the more time the rock had to form, and magma cools faster on land, not giving the rocks much time to form.
The individual grains (crystals) in quickly cooled magma are described as aphanitic--not visible without magnification.
Extrusive igneous rocks are usually fine grained.
The larger the crystals, the more time it had to cool because the crystals had more time to grow
fined grain texture