Crystalization is more of a side effect of cooling. So no.
crystallization above ground and crystallization below ground
Crystallization and cooling magma are related in the sense that cooling and crystallization occurs simultaneously. As the magma cools it crystallizes, the faster the rate of cooling the quicker crystals would develop and the slower the cooling the larger the crystals in other cases when the magma cool so rapidly crystal development may not be so prominent.
Igneous rocks are formed through two processes: cooling and solidification of molten rock (magma) on or beneath the Earth's surface (extrusive), and cooling and crystallization of magma deep beneath the Earth's surface (intrusive).
Crystallization from cooling magma is the process by which minerals solidify from a molten state as magma cools and hardens. As the magma cools, minerals crystallize at different temperatures depending on their chemical composition, leading to the formation of igneous rocks with distinct mineral compositions and textures. This process is a key mechanism driving the formation of various igneous rock types like granite, basalt, and gabbro.
When magma undergoes crystallization above ground, it forms igneous rocks known as extrusive or volcanic rocks. These rocks have fine-grained textures due to rapid cooling, and examples include basalt, andesite, and rhyolite.
phaneritic
the process of becoming hard or solid by cooling or drying or crystallization
Igneous rock
There are many factors that influence the crystallization process. Some factors are impurity level, mixing regime, vessel design, and cooling profile.
crystallization above ground and crystallization below ground
The cooling, solidification, crystallization and hardening of molten magma or lava.
Crystallization and cooling magma are related in the sense that cooling and crystallization occurs simultaneously. As the magma cools it crystallizes, the faster the rate of cooling the quicker crystals would develop and the slower the cooling the larger the crystals in other cases when the magma cool so rapidly crystal development may not be so prominent.
Rocks formed by crystallization from a melt (magma).
Yes. Cooling fan, engine fan, and radiator fan relays are all the same thing.
A coarse-grained texture typically represents a single long period of cooling and crystallization. This texture forms when the magma has had enough time to cool slowly and crystals have had time to grow to a visible size.
Heating, cooling, and crystallization can form crystals. When a solution is heated, the solubility of the solute increases, but as it cools down, the solute starts to precipitate out, forming crystals. This process is often used in various industries to purify substances or to create specific crystal structures.
obsidian :) it is used mostly as scalples because it has smooth edges unlike normal scalples they have rough blades even if you can not see them hope it helps