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- Intrusive igneous rock12345:
- Forms from magma forced into older rocks at depths within the Earth’s crust1.
- Solidifies below the Earth’s surface1.
- Examples include batholiths, dikes, sills, laccoliths, and volcanic necks2.
- Majority of igneous rocks are intrusive3.
- Characterized by large crystal sizes visible to the naked eye because they cool slowly5.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.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-rockIntrusive 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_rockIntrusive igneous rocks make up the majority of igneous rocks and are formed from magma that cools and solidifies within the crust of a planet. Bodies of intrusive rock are known as intrusions and are surrounded by pre-existing rock (called country rock).en.wikipedia.org/wiki/Igneous_rockIn 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_intrusionIntrusive (Plutonic) Rocks Intrusive igneous rocks solidify within Earth. These rocks are also known as plutonic rocks—named for Pluto, the Roman god of the underworld. Intrusive igneous rocks are generally wholly crystalline and characterized by large crystal sizes visible to the naked eye because they cool slowly.www.nps.gov/subjects/geology/igneous.htm - People also ask
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