The texture is determined by the rate it takes the molten to cool to form the rock.
The crystal texture of igneous rock is determined by the amount of time spent in cooling from magma primarily.
It depends on the size and the shape of composition
Rate of cooling of the magma, Chemical composition of the magma, Presence of volatiles.
the rate of cooling
Liquids
the length of time the magma had to cool
The length of time the magma had to cool
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.
Granite is a coarse grained igneous rock without Pyroxene.
Granular texture.
magma or lava controls most texture in igneous rock
the length of time the magma had to cool
The length of time the magma had to cool
The size of the mineral crystals in an igneous rock determines the rock's texture.
The length of time the magma had to cool
A pegmatite texture in a rock is a course-grained Igneous Rock. Granite Pegmatite is a common Igneous rock
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
fined grain texture
The texture of Andesite rock is fine-grained and it Extrusive plus it is an igneous rock .
coarse texture
The effect of weathering is to reduce the volume of the igneous rock.
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.