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.
Large grain rocks, such as granite, form from magma as it cools slowly beneath the Earth's surface. This slow cooling allows for the growth of large mineral grains within the rock. Rocks formed from lava, such as basalt, typically have much smaller grain sizes due to the rapid cooling at the Earth's surface.
it getys harder
Quartz
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.
the crystals are large
Large crystals with a coarse crystal grain texture.
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Fine
Quartz
lava
Visible or coarse.
Fine crystal grain.
When magma cools slowly within warm rock underground, it forms crystals with a coarse-grained texture. This type of crystal texture indicates that the minerals had time to grow larger before the magma solidified, reflecting a slow cooling process. Examples of rocks with coarse-grained textures include granite and diorite.
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.
Large crystalline grains.