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For the physical act of trespass with a possible intent to steal, see intruder.

Plutonic redirects here, you may have meant Platonic.

In geology an intrusion is usually a body of igneous rock that has crystallized from a molten magma below the surface of the Earth. Bodies of magma that solidify underground before they reach the surface of the earth are called plutons, named for Pluto, the Roman god of the underworld. Correspondingly, rocks of this kind are also referred to as igneous plutonic rocks.

Intrusive rocks include all varieties of igneous rocks from coarse-grained, phaneritic granites of large batholiths to very fine grained, aphanitic, rhyolites in volcanic necks or feeder pipes. In composition, intrusive rocks also include the entire sequence of igneous rock types from the dense and dark ultramafic peridotites to the very light-colored and low-density alkali granites and syenites. A well-known example of an igneous intrusion is Devil's Tower in Wyoming, USA.

Intrusive rocks also exist in a wide range of forms from mountain range sized batholiths to thin vein-like fracture fillings of aplite. Structural types include:

• batholith: large irregular intrusions.
• stock: smaller irregular disordant intrusions.
• dike: a relatively narrow tabular discordant body with near vertical attitude.
• sill: a relatively thin tabular concordant body intruded along bedding planes, horizontal attitude.
• pipe or volcanic neck: circular or tube shaped nearly vertical body which may have been a feeder vent for a volcano.
• laccolith: concorant body with essentially flat base and dome shaped upper surface, usually has a feeder pipe below.

See also

• Diapir
• Mud volcano
• Ultramafic intrusion

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