Intrusive igneous rock.
The features that form as a result of magma of magma hardening beneath the earth's surface are volcanic necks,sills and batholiths.
Igneous rocks form as a result of cooling magma. As the magma cools and solidifies, it forms rocks such as granite, basalt, and obsidian. The size of the mineral crystals in the rock is determined by the rate of cooling.
The rate of cooling of magma and lava depends on various factors such as the environment it is in, the size of the magma/lava body, and its composition. Typically, smaller lava flows cool more quickly than larger magma chambers underground. Rapid cooling can lead to the formation of fine-grained rocks like basalt, while slower cooling can result in coarser-grained rocks like granite.
No."Granite is formed by the slow cooling & crystallization of magma at some depth in the earth's crust, as indicated by its characteristic phaneritic & phaneritic-porphyritic texture."-The Audubon Society Field Guide to North American Rocks & Minerals
Yes, granite is formed underground through the slow cooling and solidification of magma beneath the Earth's surface. It is a common type of intrusive igneous rock that is often found in the continental crust.
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.
The cooling and hardening of magma deep underground results in igneous rock. Rare gems and diamonds can be found in 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.
Magma is molten rock. It becomes rock by cooling and hardening.
The features that form as a result of magma of magma hardening beneath the earth's surface are volcanic necks,sills and batholiths.
Diorite is formed by the cooling of intermediate magmas underground.
The features that form as a result of magma of magma hardening beneath the earth's surface are volcanic necks,sills and batholiths.
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.
The features that form as a result of magma of magma hardening beneath the earth's surface are volcanic necks,sills and batholiths.
When magma comes in contact with underground water, it creates hot springs, or geysers.
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.