In geology, a pluton is a body of intrusive igneous rock (also called plutonic rock) that is crystallized from magma slowly cooling below the surface of the Earth. Although pluton is a general term to describe an intrusive igneous body, there has been some confusion around the world as to the definition of a pluton. Pluton has been used to describe any non-tabular intrusive body, and batholith has been used to describe systems of plutons. In other literature, batholith and pluton have been used interchangeably. In central Europe, smaller bodies are described as batholiths and larger bodies as plutons. In practice the term pluton most often means a non-tabular igneous intrusive body. The most common rock types in plutons are granite, granodiorite, tonalite, monzonite, and quartz diorite. Generally light colored, coarse-grained plutons of these compositions are referred to as granitoids. Examples of plutons include Denali (formerly Mount McKinley) in Alaska; Cuillin in Skye, Scotland; Cardinal Peak in Washington state; Mount Kinabalu in Malaysia; and Stone Mountain in the US state of Georgia.