Pluton

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A Jurassic pluton of pink monzonite intruded below a section of gray sedimentary rocks and then was subsequently uplifted and exposed, near Notch Peak, House Range, Utah.

In geology, a pluton is a body of intrusive igneous rock (called a plutonic rock) that is crystallized from magma slowly cooling below the surface of the Earth. Plutons include batholiths, stocks, dikes, sills, laccoliths, lopoliths, and other igneous formations. In practice, "pluton" usually refers to a distinctive mass of igneous rock, typically several kilometers in dimension, without a tabular, or flat, shape like those of dikes and sills. 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.

In plutons, the most common rocks are granite, granodiorite, tonalite, monzonite, and quartz diorite. Plutons are usually light colored. Coarse-grained plutons of the last sentence's compositions are referred to as granitoids.[1]

Etymology[edit]

The name originated from the classical god of the underworld, Pluto. The use of the name was regarding the origin of basalt, and the concept goes back to earlier days of of geology in the latter 18th century, and the then hot conflict between theories of plutonism (or vulcanism), and neptunism.[1]

See also[edit]

References[edit]

  1. ^ a b . October 26, 2018 http://www.geologypage.com/2018/10/what-is-a-plutonic-igneous-rock.html. Missing or empty |title= (help)

Further reading[edit]

  • Best, Myron G. (1982). Igneous and Metamorphic Petrology. San Francisco: W. H. Freeman & Company. pp. 119 ff. ISBN 0-7167-1335-7.

External links[edit]