That is the correct US spelling of "crystallize" (also crystalize). The UK spelling is crystallise.
Magma rises when it is being pushed or heated from below.
Plutonic rocks solidify and crystallize beneath the Earth's surface. They are composed of large crystals. Volcanic rocks solidify and crystallize on the Earth's surface or under the sea. They are made up of very small crystals.
Magma is molten rock, as the magma cools the minerals crystallize out of it, the slower it cools, the larger the crystals.
Sand consists mainly of silicon dioxide, and this has a great propensity to crystallize. Sufficiently so, that in extreme circumstances actual cm-sized crystals made of sand grains are known. Sand crystals by name. In any event, because of its propensity to crystallize, SiO2 grains aggregate to form a coherent whole. This is accelerated if the sand body is subject to heat, or if it is immersed, thus making chemical bonds more easy.
Minerals that crystallize directly from seawater are examples of hydrogenous sediment.
Chocolate crystals!
Sodium chloride crystallize as face-centerd cubic crystals.
Yes. And the size of crystals depend on the time taken to crystallize.
Magma rises when it is being pushed or heated from below.
Yes, it's possible to crystallize materials out of liquids other than water.
when magma cools fast you get smaller crystals when it cools slow you get large crystals its very simple
Grape jelly contains sugar. If the product was heated too quickly, the sugars will begin to form crystals, and these crystals will continue to grow.
Plutonic rocks solidify and crystallize beneath the Earth's surface. They are composed of large crystals. Volcanic rocks solidify and crystallize on the Earth's surface or under the sea. They are made up of very small crystals.
due to slow cooling of magma within the earth causes the minerals to crystallize.
Magma is molten rock, as the magma cools the minerals crystallize out of it, the slower it cools, the larger the crystals.
The process is cooling. When magma cools slowly, large well-define crystals form.
Not usually unless you have a microscope. Crystals in baslat are usually microscopic. However, in some cases basalt may have a porphyritic texture, where some minerals in the magma have started to crystallize before the eruption.