The cooling and hardening of magma deep underground results in igneous rock. Rare gems and diamonds can be found in igneous rock.
When magma comes in contact with underground water, it creates hot springs, or geysers.
Lava will cool quickly compared to underground magma.
A coarse grained texture, referred to as a phaneritic texture, will be the resultant igneous rock texture. The slower the magma cools the more time minerals have to crystallize and thus grow bigger.
contact metamorphism
A magma chamber in a volcano is a pool-like container of liquid rock just below the earth underground. It is constantly under tremendous pressure, and with enough time, it can start fracturing rock to make places for magma to escape.
Generally, the volcano is not the result of cooling and hardening deep underground. It is the molten magma in the core of the earth that, when it rises and breaks through the earth's crust, results in volcanic action.
Intrusive igneous rock.
Intrusive igneous rocks such as dikes, sills, and batholiths are formed from the cooling and hardening of magma beneath Earth's surface. These structures are formed when magma solidifies underground, creating features like vertical dikes, horizontal sills, and large masses of magma called batholiths.
No, it would not be accurate to say that evaporation results from the cooling of magma underground. When magma cools, it solidifies into igneous rock rather than evaporating. Evaporation typically occurs when liquids turn into gases at higher temperatures, which is not the case for cooling magma. Instead, the process involves crystallization as minerals form from the cooling magma.
Magma is molten rock. It becomes rock by cooling and hardening.
Diorite is formed by the cooling of intermediate magmas underground.
The cooling, solidification, crystallization and hardening of molten magma or lava.
Igneous rocks are formed by the cooling and hardening of molten material called magma.
Quick cooling of magma results in small crystal formation. Slow cooling magma results in larger crystals.
They form underground from the cooling and solidification of magma.
Igneous
Intrusive igneous rocks, such as granite and diorite, form when magma cools underground. These rocks have a coarse-grained texture due to the slow cooling process, allowing large mineral crystals to form within the rock. Intrusive rocks are typically found in plutons or batholiths beneath the Earth's surface.