Magma is stored below the surface in reservoirs called magma chambers. It creates and follows paths called conduits to the surface. This network is often referred to as the volcano's plumbing system. These networks can cover vast areas.
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.
The mass of cooling magma is called a pluton, and the rock around is known as country rock. Slow cooling over thousands to millions of years allows large visible crystals to form. Common igneous rock types include granite, gabbro, and diorite. Large plutons can form along convergent tectonic plate boundaries.
Intrusive Igneous Features and Landforms
Batholiths are Plutons that have been exposed on the surface through uplift and erosion.
Sills and Dikes are tabular bodies of magma that intrude into a fracture. Sills follow bedding planes, whereas dikes cross-cut beds.
Monadnocks, also called Inselbergs, are isolated rock hills standing in a level plain. These are often the result of softer sedimentary rocks eroding around a hard intrusive igneous body. Devils Tower National Monument (Wyoming) is an example of a monadnock.
Intrusive Igneous Landforms in Parks
The following is a partial list of National Park Service units that include Intrusive Igneous landforms: