Plate tectonics

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The tectonic plates of the world were mapped in the second half of the 20th century.
Tectonic plates on a different map projection
Global earthquake epicenters, 1963–1998
Global plate tectonic movement

Plate tectonics [1] is a theory of geology. It has been developed to explain large scale motions of the Earth's lithosphere. This theory builds on older ideas of continental drift and seafloor spreading.[2][3]

Dissipation of heat from the mantle is the original source of energy driving plate tectonics. Exactly how this works is still a matter of debate. The driving forces of plate motion continue to be active subjects of on-going research.[4]

Earth's crust[change | change source]

The outermost part of the Earth's interior is made up of two layers. The lithosphere, above, includes the crust and the rigid uppermost part of the mantle.

Below the lithosphere is the asthenosphere. Although solid, the asthenosphere can flow like a liquid on long time scales. Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers. The deeper mantle below the asthenosphere is more rigid again. This is caused by extremely high pressure.

Thickness of plates[change | change source]

Ocean lithosphere varies in thickness. Because it is formed at mid-ocean ridges and spreads outwards, it gets thicker as it moves further away from the mid-ocean ridge. Typically, the thickness varies from about 6 kilometres (3.7 mi) thick at mid-ocean ridges to greater than 100 kilometres (62 mi) at subduction zones.[4]

Continental lithosphere is typically about 200 kilometres (120 mi) thick, though this also varies considerably between basins, mountain ranges, and stable cratonic interiors of continents. The two types of crust also differ in thickness, with continental crust being considerably thicker than oceanic (35 kilometres (22 mi) vs. 6 kilometres (3.7 mi)).[4]

Three types of plate boundaries and a hot spot

Movement of plates[change | change source]

The lithosphere consists of tectonic plates. There are eight major and many minor plates. The lithospheric plates ride on the asthenosphere. These plates move at one of three types of plate boundaries.[5][6][7][8][9]

  1. convergent boundaries.
  2. divergent boundaries.
  3. transform fault boundaries.

Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The lateral movement of the plates varies from:

  • 1–4 centimetres (0.39–1.57 in) per year (Mid-Atlantic Ridge). This is as fast as fingernails grow.
  • 10 centimetres (3.9 in) per year (Nazca Plate). This is as fast as hair grows.[10][11]

Consequences[change | change source]

Tectonic plates can create mountains, earthquakes, volcanoes, mid-oceanic ridges and oceanic trenches, depending on which way the plates are moving.

  1. together = mountains; volcanoes. The Andes mountain range in South America and the Japanese island arc are examples. Also the Pacific Ring of Fire.
  2. away = earthquakes, trenches. The Mid-ocean ridges and Africa's Great Rift Valley are examples.
  3. side to side = earthquakes. The San Andreas Fault in California is an example of a transform boundary. New Zealand is another, more complex, example.

Major plates[change | change source]

Depending on how they are defined, there are usually seven or eight major plates:

  • African Plate
  • Antarctic Plate
  • Indo-Australian Plate, sometimes subdivided into:
    • Indian Plate
    • Australian Plate
  • Eurasian Plate
  • North American Plate
  • South American Plate
  • Pacific Plate

Other pages[change | change source]

References[change | change source]

  1. from Greek τέκτων, tektōn "builder" or "mason"
  2. Oreskes, Naomi ed. 2003. Plate tectonics : an insider's history of the modern theory of the Earth. Westview Press ISBN 0-8133-4132-9
  3. Stanley, Steven M. 1999. Earth system history. Freeman. p211–228 ISBN 0-7167-2882-6
  4. 4.0 4.1 4.2 Turcotte D.L. & Schubert G. 2002. Plate tectonics in Geodynamics. 2nd ed, Cambridge University Press. 1–21 ISBN 0-521-66186-2
  5. Rolf Meissner 2002. The little book of planet Earth. New York: Copernicus Books. p202 ISBN 978-0-387-95258-1.
  6. "Plate Tectonics: Plate boundaries". platetectonics.com. http://www.platetectonics.com/book/page_5.asp. Retrieved 12 June 2010.
  7. Tackley, Paul J. (2000-06-16). "Mantle convection and plate tectonics: towards an integrated physical and chemical theory". Science 288 (5473): 2002–2007. doi:10.1126/science.288.5473.2002. PMID 10856206.
  8. Seyfert, Carl K. (1987). The Encyclopedia of Structural Geology and Plate Tectonics. ISBN 9780442281250.
  9. Oreskes (2003). Plate Tectonics : An Insider's History of the Modern Theory of the Earth. Westview Press. ISBN 9780813341329.
  10. Huang Zhen Shao (1997). "Speed of the Continental Plates". The physics factbook. http://hypertextbook.com/facts/ZhenHuang.shtml.
  11. Hancock, Paul L; Skinner, Brian J; Dineley, David L (2000). The Oxford Companion to The Earth. Oxford University Press. ISBN 0198540396.
  • McKnight, Tom 2004. Geographica: the complete illustrated atlas of the world, Barnes and Noble; New York. ISBN 0-7607-5974-X
  • Stanley, Steven M. 1999. Earth system history. Freeman, p211–228. ISBN 0-7167-2882-6
  • Thompson, Graham R. & Turk, Jonathan 1991. Modern physical geology. Saunders. ISBN 0-03-025398-5
  • Turcotte D.L. & Schubert G. 2002. Geodynamics. 2nd ed, Wiley, New York. ISBN 0-521-66624-4

Other websites[change | change source]