Small crystals or possibly no crystals at all form from rapidly cooling lava.
Yes. But larger crystals occur slower and under the crust.
no . they come from rapid cooling lava
Yes niq
True
Yes.
Your answer is true i hope this helps!!!!!
Yes they will
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.
Yes. Rapid cooling of molten rock produces small crystals.
false
Large crystals form when a rock cools from magma slowly whereas smaller crystale form when there is a slow rate of cooling
The rate at which the magma cools affects the size of the crystals that form. If it cools slowly, large crystals will form. If it cools rapidly, small crystals will form.if it takes the rock a long time to cool down the crystals will be bigger if the rock takes a short time to cool the crystals will be smaller
Yes they will
The rock cools so rapidly from magma that crystals barely have time to form.
Not enough information. Some crystals will break if they cool rapidly, some crystals will not form correctly if the solution cools too quickly.
As a general rule extrusive igneous rock crystals are very small, often microscopic, as the rock cools very rapidly. Conversely intrusive magma often cools so slowly that sizeable crystals can develop.
The size of the crystals. Large crystals mean the magma cooled slowly, small crystals are a sign that the magma was cooled quickly.
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.
Yes. Rapid cooling of molten rock produces small crystals.
false
no . they come from rapid cooling lava
Usually from the slow cooling of magma with a plentiful supply of material necessary for crystal growth, and space in which to grow.
False