Batholith

A batholith (from Greek bathos, depth + lithos, rock) is a large mass of intrusive igneous rock (also called plutonic rock), larger than 100 square kilometres (40 sq mi) in area,[1] that forms from cooled magma deep in the Earth's crust. Batholiths are almost always made mostly of felsic or intermediate rock types, such as granite, quartz monzonite, or diorite (see also granite dome).

Basic types of intrusions: 1. Laccolith
2. Small dike
3. Batholith
4. Dike
5. Sill
6. Volcanic neck, pipe
7. Lopolith
Note: As a general rule, in contrast to the active volcanic vent in the figure, these names refer to the fully cooled and usually millions-of-years-old rock formations, which are the result of the underground magmatic activity shown.
Half Dome, a granite monolith in Yosemite National Park and part of the Sierra Nevada Batholith

Formation

Although they may appear uniform, batholiths are in fact structures with complex histories and compositions. They are composed of multiple masses, or plutons, bodies of igneous rock of irregular dimensions (typically at least several kilometers) that can be distinguished from adjacent igneous rock by some combination of criteria including age, composition, texture, or mappable structures. Individual plutons are solidified from magma that traveled toward the surface from a zone of partial melting near the base of the Earth's crust.

The eroded laccolith above the batholith system of Vitosha - Plana domed mountains, next to Sofia, Bulgaria

Traditionally, these plutons have been considered to form by ascent of relatively buoyant magma in large masses called plutonic diapirs. Because the diapirs are liquified and very hot, they tend to rise through the surrounding native country rock, pushing it aside and partially melting it. Most diapirs do not reach the surface to form volcanoes, but instead they slow down, cool, and usually solidify 5 to 30 kilometers underground as plutons (hence the use of the word pluton; in reference to the Roman god of the underworld Pluto). An alternate view is that plutons commonly are formed not by ascent of large magma diapirs, but rather by aggregation of smaller volumes of magma that ascend as dikes.[2]

A batholith is formed when many plutons converge to form a huge expanse of granitic rock. Some batholiths are mammoth, paralleling past and present subduction zones and other heat sources for hundreds of kilometers in continental crust. One such batholith is the Sierra Nevada Batholith, which is a continuous granitic formation that makes up much of the Sierra Nevada in California. An even larger batholith, the Coast Plutonic Complex, is found predominantly in the Coast Mountains of western Canada; it extends for 1,800 kilometers and reaches into southeastern Alaska.

Surface expression and erosion

A batholith is an exposed area of (mostly) continuous plutonic rock that covers an area larger than 100 square kilometers (40 square miles). Areas smaller than 100 square kilometers are called stocks.[3] However, the majority of batholiths visible at the surface (via outcroppings) have areas far greater than 100 square kilometers. These areas are exposed to the surface through the process of erosion accelerated by continental uplift acting over many tens of millions to hundreds of millions of years. This process has removed several tens of square kilometers of overlying rock in many areas, exposing the once deeply buried batholiths.

Batholiths exposed at the surface are subjected to huge pressure differences between their former location deep in the earth and their new location at or near the surface. As a result, their crystal structure expands slightly over time. This manifests itself by a form of mass wasting called exfoliation. This form of weathering causes convex and relatively thin sheets of rock to slough off the exposed surfaces of batholiths (a process accelerated by frost wedging). The result is fairly clean and rounded rock faces. A well-known result of this process is Half Dome in Yosemite Valley.

Examples

Africa
  • Aswan Granite Batholith
  • Cape Coast Batholith, Ghana
  • Paarl Rock, South Africa
  • Darling Batholith, South Africa
  • Hook granite massif, Zambia
  • Mubende Batholith, Uganda

Antarctica
  • Antarctic Peninsula Batholith
  • Queen Maud Batholith

Asia

Europe
  • Revsund Massif
  • Rätan Batholith
  • Småland–Värmland Belt

North America

Oceania
  • Cullen Batholith, Australia
  • Kosciuszko Batholith, Australia
  • Moruya Batholith, Australia
  • Scottsdale Batholith, Australia [8]
  • Median Batholith, New Zealand
  • New England Batholith, Australia

South America
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See also

References
  1. Petersen, James F.; Sack, Dorothy; Gabler, Robert E. (2017). Physical Geography (11th edition). Boston: Cengage Learning Inc. p. 614. ISBN 978-1-305-65264-4.
  2. Hall, Clarence A., Jr. (2007). Introduction to the geology of southern California and its native plants. Berkeley: University of California Press. p. 22. ISBN 9780520249325.
  3. GLENCOE SCIENCE | Earth Science Twelfth Grade High School Textbook (Georgia); pg. 115 paragraph 1, pg. 521 question 9
  4. http://www.deccanchronicle.com/nation/in-other-news/010616/telangana-bhongir-fort-s-batholith-marvel.html
  5. http://suvratk.blogspot.com/2018/07/mount-abu-geology.html?m=1
  6. Douglas M. Morton, Fred K. Miller, Peninsular Ranges Batholith, Baja and Southern California, Geological Society of America, 2014
  7. Davin A. Bagdonas; Carol D. Frost; C. Mark Fanning (2016). "The origin of extensive Neoarchean high-silica batholiths and the nature of intrusive complements to silicic ignimbrites: Insights from the Wyoming batholith, U.S.A." (PDF). American Mineralogist. 101: 1332–1347. Retrieved June 8, 2016. ...Neoarchean granite batholith, herein named the Wyoming batholith, extends more than 200 km across central Wyoming in the Granite and the Laramie Mountains.
  8. Stratigraphic revision and remapping of the Mathinna Supergroup between the River Tamar and the Scottsdale Batholith, northeast Tasmania, Department of Infrastructure, Energy and Resources. Mineral Resources Tasmania. June 2011
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