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  2. Characteristics of intrusive igneous rocks12345:
    • Form below Earth's surface.
    • Slow cooling allows large crystals to form.
    • Examples include diabase, diorite, gabbro, granite, pegmatite, and peridotite.
    • Also known as plutonic rocks.
    • Intrusive features include stocks, laccoliths, sills, and dikes.
    Learn more:
    Intrusive igneous rocks crystallize below Earth's surface, and the slow cooling that occurs there allows large crystals to form. Examples of intrusive igneous rocks are: diabase, diorite, gabbro, granite, pegmatite, and peridotite. Extrusive igneous rocks erupt onto the surface, where they cool quickly to form small crystals.
    geology.com/rocks/igneous-rocks.shtml
    Intrusive igneous rocks cool underground. Deep in the crust, magma cools slowly. Slow cooling gives crystals a chance to grow. Intrusive igneous rocks have relatively large crystals that are easy to see. Intrusive igneous rocks are also called plutonic. A pluton is an igneous rock body that forms within the crust.
    k12.libretexts.org/Bookshelves/Science_and_Tech…
    Intrusive, or plutonic, igneous rock forms when magma is trapped deep inside the Earth. Great globs of molten rock rise toward the surface. Some of the magma may feed volcanoes on the Earth's surface, but most remains trapped below, where it cools very slowly over many thousands or millions of years until it solidifies.
    www.usgs.gov/faqs/what-are-igneous-rocks
    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…
    Igneous rocks which form by the crystallization of magma at a depth within the Earth are called intrusive rocks. Intrusive rocks are characterized by large crystal sizes, i.e., their visual appearance shows individual crystals interlocked together to form the rock mass.
    hyperphysics.phy-astr.gsu.edu/hbase/Geophys/intr…
     
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