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  2. Igneous intrusions form through the following processes1234:
    • Magma slowly cools below the Earth's surface, leading to the crystallization of intrusive igneous rock.
    • Intrusive rock is formed when magma penetrates existing rock and solidifies underground.
    • Types of intrusive features include batholiths, dikes, sills, laccoliths, and volcanic necks.
    • If conduits are emptied after an eruption, they can collapse to form a caldera or remain as lava tubes and caves.
    Learn more:
    In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth.
    en.wikipedia.org/wiki/Igneous_intrusion
    Intrusive rock, igneous rock formed from magma forced into older rocks at depths within the Earth’s crust, which then slowly solidifies below the Earth’s surface, though it may later be exposed by erosion.
    www.britannica.com/science/intrusive-rock
    Intrusive rock is formed when magma penetrates existing rock, crystallizes, and solidifies underground to form intrusions, such as batholiths, dikes, sills, laccoliths, and volcanic necks. Intrusion is one of the two ways igneous rock can form. The other is extrusion, such as a volcanic eruption or similar event.
    en.wikipedia.org/wiki/Intrusive_rock
    When magma cools and solidifies in these spaces, Intrusive or plutonic igneous rocks are formed deep beneath the Earth’s surface. Intrusive features like stocks, laccoliths, sills, and dikes are formed. If the conduits are emptied after an eruption, they can collapse in the formation of a caldera, or remain as lava tubes and caves.
    www.nps.gov/subjects/geology/intrusive-igneous-la…
     
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    Igneous intrusion - Wikipedia

    In geology, an igneous intrusion (or intrusive body or simply intrusion ) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and compositions, illustrated by examples like the Palisades Sill of New York and … See more

    Intrusions are broadly divided into discordant intrusions, which cut across the existing structure of the country rock, and concordant intrusions that intrude parallel to existing bedding or fabric. These are further classified … See more

    Plutonism – Geological theory that Earth's igneous rocks formed by solidification of molten material
    Salt dome – Structural dome formed of salt or halite See more

    The room problem
    The ultimate source of magma is partial melting of rock in the upper mantle and lower See more

    • Best, Myron G. (1982). Igneous and Metamorphic Petrology. San Francisco: W. H. Freeman & Company. pp. 119 ff. ISBN See more

     
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