Igneous rocks have different textures for two reasons.
The first reason is that the magma from which the igneous rocks were made can be acid (having a lot of silica in it like Granite) or basaltic (having less silica and a lot more dark minerals). The acidity of a magma has a great affect on the viscosity of the lava and this affects the texture of the rocks formed.
The second (and more important) reason relates to the speed with which the magma cools. If the magma cools quickly the crystals are small and the rocks are fine textured. If the magma cools slowly the rocks end up with big, course grained crystals.
Granite, diorite, and gabbro are examples of igneous rocks that do not have a glassy texture. These rocks are formed from slowly cooled magma underground, allowing time for crystals to grow, giving them a coarse-grained appearance.
Intrusive igneous rocks have a coarse-grained texture because they cool slowly beneath the Earth's surface, allowing larger mineral crystals to form. These rocks often have interlocking crystals that are visible to the naked eye due to their slow cooling process.
Granite
No, igneous rocks are not classified by their shape. They are primarily classified based on their origin (either intrusive or extrusive) and their texture (coarse-grained, fine-grained, glassy, etc.). Shape or form is not a major factor in the classification of igneous rocks.
An igneous rock with a coarse-grained texture forms when magma cools slowly beneath the Earth's surface, allowing large crystals to develop. This slow cooling process typically occurs in plutonic environments, such as batholiths or stocks. Common examples of coarse-grained igneous rocks include granite and diorite. The larger crystals are visible to the naked eye, distinguishing them from fine-grained rocks that cool quickly.
Granite is the name applied to coarse-grained felsic igneous rocks. These rocks are primarily composed of quartz, feldspar, and mica minerals, giving them a light color and coarse texture.
Granite, diorite, and gabbro are examples of igneous rocks that do not have a glassy texture. These rocks are formed from slowly cooled magma underground, allowing time for crystals to grow, giving them a coarse-grained appearance.
Intrusive igneous rocks are characterized by a coarse-grained texture because they cool slowly beneath the Earth's surface, allowing larger mineral crystals to form. This slow cooling process gives the minerals more time to grow, resulting in a coarse-grained appearance.
Intrusive igneous rock has a coarse, visible crystalline texture. 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. An igneous rock with a coarse texture is said to be phaneritic.
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
It is most likely formed underground.
Intrusive igneous rocks have a coarse-grained texture because they cool slowly beneath the Earth's surface, allowing larger mineral crystals to form. These rocks often have interlocking crystals that are visible to the naked eye due to their slow cooling process.
Coarse-grained texture
Coarse-grained texture
Coarse-grained texture
Granite
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.