The resultant rock would have a porphyritic texture; large crystals (usually feldspars) scattered among small crystal grains.
The texture is determined by the rate it takes the molten to cool to form the rock.
The length of time the magma had to cool
The rate at which the rock cool from the liquid magma determines their texture
No."Granite is formed by the slow cooling & crystallization of magma at some depth in the earth's crust, as indicated by its characteristic phaneritic & phaneritic-porphyritic texture."-The Audubon Society Field Guide to North American Rocks & Minerals
When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.
very coarse
smooth
They form from the extremely rapid cooling of lava or magma. The quick cooling does not allow time for the crystallization of minerals, resulting in the formation of a natural glass.
It's texture is porphyritic
Small crystal grains form from rapid cooling of magma resulting in an aphanitic rock texture.
The texture is determined by the rate it takes the molten to cool to form the rock.
Slow cooling of magma far beneath earth's surface has a phaneritic texture (this means that the individual crystals are large enough to be seen with the naked eye).
Quick cooling of magma results in small crystal formation. Slow cooling magma results in larger crystals.
The length of time the magma had to cool
Porphyritic texture indicates that a magma has gone through a two stage cooling process. The magma has cooled sufficiently underground to allow some minerals to crystallize and grow in size; the magma is then expelled above ground where the remaining liquid magma solidifies quickly, allowing only small crystals to develop.
The slow cooling of magma far beneath earth's surface creates the rock inside earth to change slowly... this means that earths surface changes in times because of this cooling magma.
They form from the extremely rapid cooling of lava or magma. The quick cooling does not allow time for the crystallization of minerals, resulting in the formation of a natural glass.