large crystals
they are huge or big
1. the coarse grained rock 2. slow cooling magma 3. fine grained rock
Magma cooling beneath the surface creates intrusive igneous rocks.
The slow cooling of magma far beneath earth's surface creates the rock inside earth to change slowly... this means that earths surface changes in times because of this cooling magma.
Igneous
Granite
Quick cooling of magma results in small crystal formation. Slow cooling magma results in larger crystals.
large crystals
1. the coarse grained rock 2. slow cooling magma 3. fine grained rock
Basalt is formed from relatively rapid cooling magma.
The rate of cooling is the speed at which magma or lava crystallizes. When the speed is slow it results in big crystals. When the speed is fast it results in small crystals.
slow cooling of gaseous magma
Gabbro is formed from slow cooling basaltic magma.
Magma cooling beneath the surface creates intrusive igneous rocks.
When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.
The slow cooling of magma far beneath earth's surface creates the rock inside earth to change slowly... this means that earths surface changes in times because of this cooling magma.
Granite and Gabbro.
A laccolith.