magma can be classified into two,magma of granitic composition(originates from lower continental crust) and magma of basaltic composition (which originates from upper mantle).Both can form intrusive rocks.
Intrusive igneous rocks.
Plutonic (intrusive) igneous rock
No, intrusive rock is not also called platonic rock. Plutonic rock is another name for this type of rock, which is produced by magma.
Igneous rocks form from the solidification of magma. This process can occur either underground (intrusive igneous rocks) or at the surface (extrusive igneous rocks), depending on the cooling rate of the magma. Examples of igneous rocks include granite, basalt, and obsidian.
MetamorphicPlutonic rocks, (Intrusive igneous rocks).
Igneous rocks can be either extrusive or intrusive. Extrusive igneous rocks form from lava cooling quickly on or near the Earth's surface, resulting in small crystals. Intrusive igneous rocks form from magma cooling slowly beneath the Earth's surface, resulting in larger crystals.
Yes, if magma crystallizes below Earth's surface it will form igneous rocks like granite or diorite. These rocks are known as intrusive igneous rocks, as they formed from magma that cooled and solidified within the Earth's crust.
Igneous rock can be both intrusive and extrusive. Intrusive igneous rocks form from magma that cools beneath the Earth's surface, while extrusive igneous rocks form from lava that cools on the Earth's surface. Examples of intrusive igneous rocks include granite and diorite, while examples of extrusive igneous rocks include basalt and rhyolite.
Intrusive igneous rocks are formed from slow cooling of magma. The additional time spent in a liquid state allows for the creation of larger mineral crystals. A rock with larger mineral crystals is said to have a coarse texture.
Igneous, Metamorphic, and Sedimentary rocks
Intrusive igneous rocks are formed from magma that cools and solidifies beneath the Earth's surface, resulting in a coarse-grained texture. Examples of intrusive igneous rocks include granite and diorite. They are characterized by their larger crystal size, which are a result of the slow cooling process.
Magma forms igneous rock when it cools and hardens. Igneous rocks can be further classified as intrusive (formed below the surface) or extrusive (formed on the surface).