Quartz
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.
Grain refers to particle or crystal size in rock.
The crystal grain size of dolomite typically ranges from very fine to fine. Dolomite is a mineral composed of calcium magnesium carbonate and is commonly found in sedimentary rocks. The size of its crystals can vary depending on the specific geological conditions under which it forms.
Grain size typically increases by a factor of 2-4 for each texture category. For example, from fine to medium grain size, there is a doubling or quadrupling of grain size. This progression helps geologists classify rocks based on their crystal sizes.
fine grained or coarse grained
Visible or coarse.
Large crystals with a coarse crystal grain texture.
It is mineral
Fine
Quartz
the crystals are large
lava
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.
When molten rock cools quickly, fine-grained crystals form. This happens because there is not enough time for larger crystals to grow before the rock solidifies, resulting in smaller crystals being formed.
Small crystal grains form when molten rock cools quickly. In an extrusive igneous rock, it's referred to as aphanitic texture.