When molten rock cools slowly, it will have a lot of time to form crystals, so the crystal size will be quite big. Take granite, for example. With the naked eye, you can see the individual crystals. The grain size is quite large.
The kind of mineral that forms is dependent on the composition of the magma.
When magma cools quickly, small crystals, or in some cases, no crystals are formed in the resultant rock.
Comparatively small crystals form from rapidly cooling magma.
Rapid cooling leads to fine crystals. This produces an aphanitic texture in igneous rocks.
Not sure about your use of "crystals", but when lava cools quickly, it makes a volcanic glass called "obsidian".
fine grain
Quartz
Grain refers to particle or crystal size in rock.
granite's crystal size varies from 1 mm to 10 mm
it getys harder
The rate at which the lava or magma cools affects the grain size, or texture, of the rock. The faster a rock cools, the smaller the individual mineral grains within it remain. Examples are basalt and rhyolite, which cooled on the earth's surface and are very fine-grained and therefore have a finer texture. But the slower a rock cools, the larger the individual mineral grains within it can grow. The best example is granite, a very coarse-textured rock that cooled very slowly deep within the earth.
the crystals are large
Large crystals with a coarse crystal grain texture.
It is mineral
Fine
Quartz
As magma cools slowly, large coarse crystals form. This is described as a phaneritic texture.
The crystal can be fine like Obseidian
lava
Visible or coarse.
Fine crystal grain.
Small crystal grains form from rapid cooling of magma resulting in an aphanitic rock texture.
The texture of the rock product of slow cooling magma is referred to as coarse grained.