Types of Intrusive Igneous Bodies

Intrusive igneous bodies are formed when magma cools and solidifies beneath the Earth's surface. Magma is less dense than the surrounding rock, so it tends to rise towards the surface. If it encounters a crack or weakness in the rock, it can intrude into the surrounding rock and form an intrusive igneous body.

In most cases, a body of hot magma is less dense than the rock surrounding it, so it has a tendency to creep upward toward the surface. It does so in a few different ways:

  • Filling and widening existing cracks
  • Melting the surrounding rock (called country rock)
  • Pushing the rock aside (where the rock is hot enough and under enough pressure to deform without breaking)
  • Breaking the rock.

When magma forces itself into cracks, breaks off pieces of rock, and then envelops them, this is called stoping. The resulting fragments are called xenoliths.

Plutons can have different shapes and different relationships with the surrounding country rock. These characteristics determine what name the pluton is given.

Types of Intrusive Igneous Bodies
Types of Intrusive Igneous Bodies. Plutons can have a variety of shapes, and be positioned in a variety of ways relative to the surrounding rocks. They are named according to these characteristics. [Karla Panchuk CC-BY-ND 4.0]

Large, irregularly shaped plutons are called stocks or batholiths, depending on size. Tabular plutons are called dikes if they cut across existing structures, and sills if they do not. Laccoliths are like sills, except they have caused the overlying rocks to bulge upward. Pipes are cylindrical conduits.

Types of Plutons

Intrusions can be classified according to the shape and size of the intrusive body and its relation to the other formations into which it intrudes:


Batholiths are the largest type of intrusive igneous body, with a surface area of greater than 100 square kilometers. They are typically formed from the crystallization of large volumes of magma. Think of them as giant underground mountains of granite, diorite, or other felsic (silica-rich) rocks. Batholiths often form during mountain building events due to the melting of continental crust.


A chonolith is a large, cylindrical intrusive igneous body that is more than 100 square kilometers in area. Chonoliths are thought to form when magma rises from the mantle and intrudes into surrounding rocks. The magma can solidify in the cylinder, forming a chonolith.


A cupola is a small, mushroom-shaped intrusive igneous body that is typically less than 1 square kilometer in area. Cupolas are often found in the central parts of larger intrusive igneous bodies, such as batholiths. Cupolas are typically composed of more felsic (silica-rich) igneous rocks than the surrounding rocks.


Dikes are vertical or steeply dipping intrusive igneous bodies that form when magma intrudes into cracks in the rock. They can be very thin, just a few centimeters wide, or very thick, up to hundreds of meters. Dikes are often composed of mafic (silica-poor) igneous rocks like basalt.


Laccoliths are dome-shaped intrusive igneous bodies that form when magma intrudes into a layer of rock, pushing the overlying rock upwards. They are typically composed of felsic or intermediate igneous rocks, such as granite or syenite. Laccoliths can be important sources of mineral resources, such as copper, molybdenum, and uranium.


Lopoliths are intrusive igneous bodies that have a saucer-shaped shape. They form when magma intrudes into the Earth's crust and spreads out laterally, pushing the overlying rock down. Lopoliths are often composed of mafic igneous rocks, such as basalt or gabbro. They can be important sources of platinum group elements (PGEs) and other valuable minerals.


A concordant lens-shaped pluton that typically occupies the crest of an anticline or trough of a syncline. They are typically composed of felsic or intermediate igneous rocks, such as granite or diorite. Phacoliths can be important markers of past tectonic activity and can provide insights into the history of deformation in an area.

Volcanic pipe or volcanic neck

tubular roughly vertical body that may have been a feeder vent for a volcano


Sills are horizontal or gently dipping intrusive igneous bodies that form when magma intrudes between layers of existing rock.


Stocks are similar to batholiths, but they are smaller, with a surface area of less than 100 square kilometers. Examples of stocks include the Henry Mountains of Utah and the Shiprock in New Mexico.


A small stock. A boss is a small, dome-shaped intrusive igneous body that is less than 100 square kilometers in area. Bosses are often found in groups, and they can be formed when magma intrudes into overlying rocks and pushes them up into a dome shape. Bosses are often found in areas of volcanic activity, and they can be composed of a variety of igneous rocks, including granite, gabbro, and diorite.

Types of Intrusive Igneous Rock
Hosta Beach rock formations - North Uist, Outer Hebrides, Scotland

Plutonic Igneous Bodies Characteristics

A body of intrusive igneous rock which crystallizes from magma cooling underneath the surface of the Earth is called a pluton. If the pluton is large, it may be called a batholith or a stock depending on the area exposed at the surface.

If the body has an exposed surface area greater than 100 km2, then it’s a batholith, otherwise it’s a stock. Batholiths are typically formed when a number of stocks coalesce beneath the surface to create one large body.

Intrusive rocks are characterized by large crystal sizes, and as the individual crystals are visible, the rock is called phaneritic. Tabular (sheet-like) plutons are classified according to whether or not they are concordant with (parallel to) existing layering (e.g., sedimentary bedding or metamorphic foliation) in the country rock

This is as the magma cools underground, and while cooling may be fast or slow, cooling is slower than on the surface, so larger crystals grow. If it runs parallel to rock layers, it is called a sill.  A sill is concordant with existing layering, and a dike is discordant. If the country rock has no bedding or foliation, then any tabular body within it is a dike. Note that the sill-versus-dike designation is not determined simply by the orientation of the feature. A dike could be horizontal and a sill could be vertical- it all depends on the orientation of features in the surrounding rocks.

If an intrusion makes rocks above rise to form a dome, it is called a laccolith. A laccolith is a sill-like body which has expanded upward by deforming the overlying rock.

A pipe, as the name suggests, is a cylindrical body with a circular, ellipitical, or even irregular cross-section, which serves as a conduit (or pipeline) for the movement of magma from one location to another. Pipes may feed volcanoes, but pipes can also connect plutons. It is also possible for a dike to feed a volcano.

How deep-seated intrusions burst through the overlying strata causes intrusive rock to be recognized: Veins spread out into branches, or branchlike parts result from filled cracks, and the high temperature is evident in how they alter country rock. As heat dissipation is slow, and as the rock is under pressure, crystals form, and no vitreous rapidly chilled matter is present.

The intrusions did not flow while solidifying, hence do not show lines. Contained gases could not escape through the thick strata, thus form cavities, which can often be observed. Because their crystals are of the rough equal size, these rocks are said to be equigranular.

Intrusive rocks formed at greater depths are called plutonic or abyssal. Some intrusive rocks solidified in fissures as dikes and intrusive sills at shallow depth and are called subvolcanic or hypabyssal. They show structures intermediate between those of extrusive and plutonic rocks. They are very commonly porphyritic, vitreous, and sometimes even vesicular. In fact, many of them are petrologically indistinguishable from lavas of similar composition.

The most obvious effect that country rock can have on magma is a chilled margin along the edges of the pluton. The country rock is much cooler than the magma, so magma that comes into contact with the country rock cools much faster than magma toward the interior of the pluton. Rapid cooling leads to smaller crystals, so the texture along the edges of the pluton is different from that of the interior of the pluton, and the colour may be different.

Intrusive igneous bodies are also important sources of mineral resources. Many metallic and non-metallic minerals are concentrated in intrusive igneous rocks. For example, copper, gold, and silver are often found in porphyritic intrusions. And tin, lithium, and tantalum are often found in pegmatitic intrusions.

See also:
What Gems Are Found in Igneous Rock?
General Classification of Igneous Rocks
The Texture of Igneous Rocks
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