True
Slow cooling magma far beneath Earth's surface is called intrusive or plutonic igneous rock. This process allows minerals to grow larger due to the slower cooling rate, resulting in a coarse-grained texture. Examples include granite and diorite.
It is called geothermal energy.
Extrusive rocks are formed outside of earths surface. Intrusive rocks are formed inside earths surface.
Obsidian
batholith!! :)
Slow cooling magma far beneath Earth's surface is called intrusive or plutonic igneous rock. This process allows minerals to grow larger due to the slower cooling rate, resulting in a coarse-grained texture. Examples include granite and diorite.
crust
it is called magma.
crust
magma
The point beneath the earth's surface where an earthquake originates is called the hypocenter.
It is called geothermal energy.
it is called magma.
Well water
which are the following?
The two most common types of rock beneath the Earth's crust are basalt and granite. Basalt is an extrusive igneous rock that forms from the cooling of magma on the Earth's surface, while granite is an intrusive igneous rock that forms from the slow cooling of magma beneath the Earth's surface.
1800km - 1900km