It depends on if it is intrusive or extrusive.
If it is an intrusive rock, it is formed when magma hardens under the earth and has a larger grain size.
If it is an extrusive rock, it is formed when lava hardens on the earth's surface and has a smaller grain size.
The cooling rate of magma primarily controls the grain size of igneous rock. Faster cooling results in smaller grains, while slower cooling leads to larger grains. Other factors that can influence grain size include the composition of the magma and the amount of gas or water present during solidification.
Basalt and gabbro are both igneous rocks, with major differences in grain size and where they form. Basalt has fine-grained crystals and forms from lava flows on the Earth's surface, while gabbro has coarse-grained crystals and forms from magma cooling beneath the Earth's surface.
All three rock types are found in continental crust, with a preponderance of granitic type igneous rock.
The grain size of an extrusive igneous rock is typically fine-grained to aphanitic, meaning the individual mineral grains are not visible to the naked eye. This rapid cooling at the Earth's surface prevents large crystals from forming, resulting in a fine texture.
An intrusive igneous rock.
The cooling rate of magma primarily controls the grain size of igneous rock. Faster cooling results in smaller grains, while slower cooling leads to larger grains. Other factors that can influence grain size include the composition of the magma and the amount of gas or water present during solidification.
fined grain texture
it means unfoliated that's my answer
it getys harder
Phaneritic refers to igneous rock grain size,which is visible with the naked eye.
Igneous rocks have a wide range of strengths depending on factors like mineral composition and cooling history. Some igneous rocks, like granite, can be very strong and durable, while others, like pumice, can be quite weak and easily crumble.
The rate of cooling is the main factor that controls texture in igneous rocks. Faster cooling leads to fine-grained textures, while slower cooling leads to coarse-grained textures. Other factors that can influence texture include the mineral composition of the magma and the presence of gases or water vapor during solidification.
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
Gabbro.
Smooth and shiny with no visible grain.
Gneiss which is a non-foliated meta-igneous rock is coarse grained in texture.
Yes, basalt is an igneous rock. it comes from when the volcano erupts. it is the hardened lava. a main factor is silica.