No. Small crystals form.
Pumice is made of glass. Glass forms when molten rock cools too quickly for crystals to form.
igneous Extrusive is cool on the outside of the crust and cools quickly before crystal forms igneous Intrusive is cool on the inside of the crust and cools slowly and allowing crystal to form
large ones
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.
Crystals are made from molten magma that cools causing silicate minerals to crystallize. The different crystal shapes form differently as the magma cools at different rates.
Large mineral crystals can form when magma is able to cool slowly underground, creating intrusive igneous rock.
Fine crystal grain.
Small crystal grains form when molten rock cools quickly. In an extrusive igneous rock, it's referred to as aphanitic texture.
If lava cools quickly, the minerals don't have as much time to form crystals, so the crystals do not become very large. Igneous rocks that cooled quickly and have small crystals are described as "aphanitic" igneous rocks.
Not enough information. Some crystals will break if they cool rapidly, some crystals will not form correctly if the solution cools too quickly.
Pumice doesn't have crystals at all, as it cools too quickly for them to form.
Usually from the slow cooling of magma with a plentiful supply of material necessary for crystal growth, and space in which to grow.
If rock cools quickly it does not have time to form large crystals and so it forms small ones. At slower cooling rates there is time to form larger crystals.
If the magma cools down fastly the crystal size is small because the crystals do not have much time to form. If They magma slows down slowly the crystal size is big because it gives the crystals time to form! :D
Small crystal grains form from rapid cooling of magma resulting in an aphanitic rock texture.
Pumice is made of glass. Glass forms when molten rock cools too quickly for crystals to form.
As magma cools slowly, large coarse crystals form. This is described as a phaneritic texture.