The slower a mineral cools, the larger the crystals it forms. Rapid cooling produces fine grained rocks / minerals, while slow cooling produces large grained rocks / minerals.
In the case of igneous rocks, for example, you can tell whether it was formed inside the earth and underwent slow cooling (like granite) or was formed during extrusion from the earth, (such as during a volcanic eruption), which would expose it to water or air, cooling it rapidly.
If it has large, chunky crystals, in is an intrusive rock, formed inside the earth, and cooled very slowly. If it is very fine grained or has no grains, (such as obsidian), it is an extrusive rock.
Rapid cooling of lava in which tiny crystals form results in a glassy texture.
It is likely to have a coarse-grained texture.
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.
the rate melted rock cools.
The texture is determined by the rate it takes the molten to cool to form the rock.
Quick cooling of magma results in small crystal formation. Slow cooling magma results in larger crystals.
smooth
Rapid cooling of lava in which tiny crystals form results in a glassy texture.
They are said to have a glassy or vitreous texture.
The texture is mostly determined by the time spent in cooling from magma or lava. The quicker the transition from molten to solid, the finer the texture.
It is likely to have a coarse-grained texture.
phaneritic
phaneritic
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.
The texture is determined by the rate it takes the molten to cool to form the rock.
the rate melted rock cools.
The texture would be glass-like.