due to slow cooling of magma within the earth causes the minerals to crystallize.
Yes. All intrusive igneours rocks and many extrusive rocks have crystals.
Intrusive Rocks are found underneath Earths crust, while Extrusive rocks are found above Earths crust.
No. Intrusive igneous rocks have large crystals because they cool slowly.
Coarse crystals are found in intrusive rocks because these rocks form from magma that cools and solidifies slowly beneath the Earth's surface. The prolonged cooling period allows individual mineral crystals ample time to grow larger, resulting in the coarse texture characteristic of intrusive igneous rocks, such as granite. In contrast, extrusive rocks cool quickly on the surface, leading to finer-grained textures.
Typically, intrusive crystals are larger than extrusive crystals because intrusive rocks cool slowly beneath the Earth's surface, allowing larger crystals to form, while extrusive rocks cool quickly at the surface, producing smaller crystals.
If a rock has large crystals, it is an intrusive rock. Intrusive rocks form underneath the Earth's surface. Magma cools slowly so it has time to form large crystals. An example is granite, where you can see the crystals with your naked eye. Rocks that have small crystals are extrusive rocks. Extrusive rocks are ones that form from lava (blasted out of a volcano) so they cool very quickly, not allowing large crystals to form. An example is obsidian, where you cannot visibly see the small crystals; it just looks like one black, glassy rock.
Intrusive igneous rocks tend to be coarser in texture because they form from magma that cools slowly beneath the Earth's surface, allowing larger mineral crystals to grow. In contrast, extrusive igneous rocks cool quickly on the surface, resulting in a finer texture with smaller crystals. Therefore, if larger mineral crystals are present, they are typically found in intrusive igneous rocks.
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
Generally, false. Intrusive rocks cool far more slowly than extrusive ones, so the crystals have time to grow larger.
Large crystals are typically characteristic of intrusive igneous rocks, which form beneath the Earth's surface from slow cooling of magma. Extrusive igneous rocks cool quickly at or near the Earth's surface, resulting in smaller crystals or glassy textures.
Extrusive rocks that cool more rapidly than intrusive rocks generally have a fine-grained texture with small mineral crystals. This rapid cooling prevents larger crystals from forming due to lack of time for crystal growth. Examples of such rocks include basalt and rhyolite.
The longer that magma is able to cool, the larger the crystals will be. Intrusive rocks will have larger crystals than extrusive rocks. For example granite (intrusive) has larger grains than rhyolite (extrusive).