Sounds like you're studying rocks in science too!
It's called porphyry. Glad to help a fellow student out ;)
Slower cooling allows the atoms time to arrange in a crystalline form, whereas faster cooling freezes the atoms in position before they can all arrange themselves in the crystalline structure.
Crystal size in these rock types is determined by their rate of cooling. Pegmatites have large crystals due to very slow cooling. Obsidian has microscopic crystals due to almost instantaneous cooling.
large,well developed crystals.This is because of slow cooling process
Does slower cooling result in bigger crystals
A slow rate of cooling. The slower a magma cools, the longer the crystals have to grow, thus the bigger they will be.
because the crystals gradually start to melt.
Crystals that are formed below the surface are formed by the cooling of magma. Crystals above the surface are formed when a volcano erupts, and cools, again, above the surface. Crystals that are below the surface usually have a slower rate of cooling than those above the surface, causing bigger crystals because of the slower cooling:)
Fast cooling=small crystals Slow cooling=big crystals
I think (and know) it is because there is less time for crystals to grow.
Slower cooling allows the atoms time to arrange in a crystalline form, whereas faster cooling freezes the atoms in position before they can all arrange themselves in the crystalline structure.
fast cooling rate forms smaller crystals eg Andesiteslow cooling rate forms large crystals eg.Pegmatite
Slow cooling of igneous rocks typically forms large crystal grains. This is because slow cooling allows more time for mineral grains to grow, resulting in larger crystals. Examples of rocks formed through slow cooling and having large crystal grains include granite and gabbro.
Crystal size in these rock types is determined by their rate of cooling. Pegmatites have large crystals due to very slow cooling. Obsidian has microscopic crystals due to almost instantaneous cooling.
Yes steel can have multiple types of crystalline structure or "grain" structure. These structures can be changed by heating and cooling the steel in particular ways. This is not unlike how different temperatures and cooling speeds cause water to form different sizes and shapes of ice crystals, which can be readily observed in snow crystals. In steel, the properties of the alloy will be determined in large part by the crystal structure, like hardness, ductility, tensile strength. The manipulation of these crystalline structure through controlled heating and cooling is known as tempering, or heat treating.
The larger the crystals, the more time it had to cool because the crystals had more time to grow
It depends on the cooling of lava. Slow cooling forms big crystals deep under the surface while fast cooling creates small crystals on or just below the earths surface. Itstant cooling wouls have no crystals.
large crystals