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Antarctic plate

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Major tectonic plate containing Antarctica and the surrounding ocean floor

Antarctic plate
TypeMajor
Approximate area60,900,000 km2 (23,500,000 sq mi)[1]
Movement1South-west
Speed112–14 mm (0.47–0.55 in)/year
FeaturesAntarctica,Kerguelen Plateau,Southern Ocean
1Relative to theAfrican plate

TheAntarctic plate is atectonic plate containing thecontinent ofAntarctica, theKerguelen Plateau, andsome remote islands in theSouthern Ocean and other surroundingoceans. After breakup fromGondwana (the southern part of thesupercontinentPangea), the Antarctic plate began moving the continent of Antarctica south to its present isolated location, causing the continent to develop a much colder climate.[2] The Antarctic plate is bounded almost entirely by extensionalmid-ocean ridge systems. The adjoining plates are theNazca plate, theSouth American plate, theAfrican plate, theSomali plate, theIndo-Australian plate, thePacific plate, and, across atransform boundary, theScotia andSouth Sandwich plates.

The Antarctic plate has an area of about 60,900,000 km2 (23,500,000 sq mi).[3] It is Earth's fifth-largest tectonic plate.

The Antarctic plate's movement is estimated to be at least 1 cm (0.4 in) per year towards theAtlantic Ocean.[4]

Subduction beneath South America

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The Antarctic plate started tosubduct beneath South America 14 million years ago in theMiocene epoch. At first it subducted only in the southernmost tip ofPatagonia, meaning that theChile triple junction lay near theStrait of Magellan. As the southern part of theNazca plate and theChile Rise became consumed by subduction the more northerly regions of the Antarctic plate began to subduct beneath Patagonia so that the Chile triple junction lies at present in front ofTaitao Peninsula at 46°15' S.[5][6] The subduction of the Antarctic plate beneath South America is held to have upliftedPatagonia as it reduced the previously vigorous down-dragging flow in theEarth's mantle caused by the subduction of theNazca plate beneath Patagonia. Thedynamic topography caused by this uplift raisedQuaternary-agedmarine terraces and beaches across the Atlantic coast of Patagonia.[6]

Land

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References

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  1. ^"Sizes of Tectonic or Lithospheric Plates". Geology.about.com. March 5, 2014. Archived fromthe original on June 5, 2016. RetrievedJanuary 22, 2016.
  2. ^Fitzgerald, Paul (2002)."Tectonics and landscape evolution of the Antarctic plate since the breakup of Gondwana, with an emphasis on the West Antarctic Rift System and the Transantarctic Mountains"(PDF).Royal Society of New Zealand Bulletin (35):453–469. RetrievedFebruary 1, 2015.
  3. ^Wohletz, K.H.; Brown, W.K."SFT and the Earth's Tectonic Plates". Los Alamos National Laboratory. Archived fromthe original on February 17, 2013.
  4. ^Jiang, Wei-Ping; E, Dong-Chen; Zhan, Bi-Wei; Liu, You-Wen (2009). "New Model of Antarctic plate Motion and Its Analysis".Chinese Journal of Geophysics.52 (1):23–32.doi:10.1002/cjg2.1323.ISSN 2326-0440.
  5. ^Cande, S.C.; Leslie, R.B. (1986). "Late Cenozoic Tectonics of the Southern Chile Trench".Journal of Geophysical Research: Solid Earth.91 (B1):471–496.Bibcode:1986JGR....91..471C.doi:10.1029/JB091iB01p00471.
  6. ^abPedoja, Kevin; Regard, Vincent; Husson, Laurent; Martinod, Joseph; Guillaume, Benjamin; Fucks, Enrique; Iglesias, Maximiliano; Weill, Pierre (2011)."Uplift of quaternary shorelines in eastern Patagonia: Darwin revisited"(PDF).Geomorphology.127 (3–4):121–142.Bibcode:2011Geomo.127..121P.doi:10.1016/j.geomorph.2010.08.003.
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