Agfdhyk

Half Dome, a granite monolith in Yosemite National Park and part of the Sierra Nevada Batholith

This article includes a list of references, but its sources remain unclear because it has insufficient inline citations. Please help to improve this article by introducing more precise citations. (March 2015) (Learn how and when to remove this template message)

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 smoldering 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.

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


• Darling Batholith, South Africa


• 
  Hook granite massif, Zambia


• Mubende Batholith, Uganda

Antarctica

• Antarctic Peninsula Batholith


• Queen Maud Batholith

Asia

• 
  Angara-Vitim batholith, Siberia


• 
  Bhongir Fort Batholith, Telangana, India^[4]
  


• 
  Gangdese batholith, Himalaya


• Trans-Himalayan Batholith, Himalaya


• 
  Kalba-Narym batholith, Kazakhstan


• Karakorum Batholith, Himalaya


• Tak batholith, Thailand


• Tien Shan batholith, Central Asia

Europe

• Bindal Batholith, Norway


• 
  Cornubian batholith, England


• Corsica-Sardinia Batholith


• 
  Donegal batholith, Ireland


• Leinster Batholith, Ireland


• Mancellian batholith, France


• 
  North Pennine Batholith, England


• 
  Ljusdal Batholith, Sweden


• Mt-Louis-Andorra Batholith


• Riga Batholith, Latvia


• Salmi Batholith, Republic of Karelia, Russia


• Sunnhordaland Batholith, Norway


• 
  Transscandinavian Igneous Belt, Sweden and Norway

• Revsund Massif


• Rätan Batholith


• Småland–Värmland Belt

North America

• Bald Rock Batholith


• Boulder Batholith


• British Virgin Islands


• Chambers-Strathy Batholith


• 
  Town Mountain Granite batholith, Texas


• Golden Horn Batholith


• Idaho Batholith


• Ilimaussaq Batholith, Greenland
  


• Kenosha Batholith


• Ruby Mountains


• Rio Verde Batholith, Mexico


• Sierra Nevada Batholith


• South Mountain Batholith, Nova Scotia


• 
  Peninsular Ranges, Baja and Southern California^[5]
  


• Stone Mountain


• Pike's Peak Granite Batholith


• Chilliwack batholith


• 
  Wyoming batholith^[6]
  

Oceania

• Cullen Batholith, Australia


• 
  Kosciuszko Batholith, Australia


• 
  Moruya Batholith, Australia


• Median Batholith, New Zealand


• New England Batholith, Australia

South America

• 
  Achala Batholith, Argentina


• 
  Antioquia Batholith, Colombia


• Guanambi Batholith, Bahia, Brazil


• 
  Parguaza rapakivi granite Batholith, Venezuela and Colombia


• 
  Cerro Aspero Batholith, Argentina


• Coastal Batholith of Peru


• 
  Colangüil Batholith, Argentina


• 
  Cordillera Blanca Batholith, Peru


• 
  Vicuña Mackenna Batholith, Chile


• 
  Elqui-Limarí Batholith, Chile and Argentina


• 
  Futrono-Riñihue Batholith, Chile


• 
  Illescas Batholith, Uruguay


• Coastal Batholith of central Chile


• 
  Panguipulli Batholith, Chile


• Patagonian Batholith, Chile and Argentina
  
  
  
  • North Patagonian Batholith
  
  
  • South Patagonian Batholith
  
  
  
  

See also

• Laccolith


• Sill


• Stock


• Volcanic plug

References

• Plummer, McGeary, Carlson, Physical Geology, Eighth Edition (McGraw-Hill: Boston, 1999) pages 61–63
  ISBN 0-697-37404-1
  


• Glazner, Bartley, Coleman, Gray, Taylor, Are plutons assembled over millions of years by amalgamation from small magma chambers?, GSA Today: Vol. 14, No. 4, pp. 4–11

External links

• Idaho Batholith


• The Cornubian Batholith