pegmatitic
Coarse
It is most likely formed underground.
The texture would be glass-like.
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 texture of intrusive igneous rocks is phaneritic, which is characterized by coarse-grained large crystals that are visible to the naked eye. The texture of volcanic rocks, meanwhile, is porphyritic, which is characterized by fine-grained crystals.
Coarse
It is most likely formed underground.
The texture would be glass-like.
You could determine whether the rock cooled underground or above the surface.
Intrusive igneous rock is composed of visible mineral crystals, possessing what is referred to as a phaneritic texture. This is evidence that slow cooling of magma occurred deep underground.
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
The rock would have visible mineral crystals--a phaneritic texture.
magma or lava controls most texture in igneous rock
Crystalline texture.
fined grain texture
The size of the mineral crystals in an igneous rock determines the rock's texture.
A porphyritic texture can be a feature of igneous rocks, but 'porphyritic' is not used to describe metamorphic rock texture. Metamorphic rocks can be foliated or non-foliated, terms used to describe mineral alignment or banding, or the lack thereof.