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[[File:South American plates.png|thumb|right|300px|{{legend|#C2E8E4|The Nazca plate, shown in light blue|border=#000 solid 1px}}<center>[http://commons.wikimedia.org/wiki/File:Plates_tect2_en.svg Full-size image showing all plates]</center>]]


The '''Nazca Plate''', named after the [[Nazca]] region of southern [[Peru]], is an oceanic [[tectonic plate]] in the eastern [[Pacific Ocean]] basin off the west coast of [[South America]]. The ongoing [[subduction]], along the [[Peru-Chile Trench]], of the Nazca Plate under the [[South American Plate]] is largely responsible for the [[Andes|Andean orogeny]]. The Nazca Plate is bounded on the west by the [[Pacific Plate]] and to the south by the [[Antarctic Plate]] through the [[East Pacific Rise]] and the [[Chile Rise]] respectively. The movement of the Nazca Plate over several [[hotspot (geology)|hotspots]] has created some [[volcanic islands]] as well as east-west running [[seamount]] chains that subduct under South America. Nazca is a relatively young plate both in terms of the age of its rocks and its existence as an independent plate{{clarify|date=April 2013}}.


==Boundaries==
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===East Pacific and Chile Rise===
{{Main|East Pacific Rise|Chile Rise}}
A [[triple junction]], the [[Chile Triple Junction]],<ref>http://www.nsm.buffalo.edu/courses/gly481-581/McGuire05_2.pdf Tectonics of South America: Chile Triple Junction</ref> occurs on the seafloor of the [[Pacific Ocean]] off [[Taitao Peninsula|Taitao]] and [[Tres Montes Peninsula]] at the southern coast of [[Chile]]. Here three [[tectonics|tectonic]] plates meet: the Nazca Plate, the [[South American Plate]], and the [[Antarctic Plate]].
 
===Peru-Chile Trench===
{{See also|Peru-Chile Trench}}
 
The eastern margin is a [[convergent boundary]] [[subduction zone]] under the South American Plate and the [[Andes Mountains]], forming the [[Peru-Chile Trench]]. The southern side is a [[divergent boundary]] with the Antarctic Plate, the [[Chile Rise]], where [[seafloor spreading]] permits [[magma]] to rise. The western side is a divergent boundary with the [[Pacific Plate]], forming the [[East Pacific Rise]]. The northern side is a divergent boundary with the [[Cocos Plate]], the [[Galapagos Rise]].
 
The subduction of the Nazca plate under southern Chile has a history of producing massive earthquakes, including the largest ever recorded on earth, the [[moment magnitude scale|moment magnitude]] 9.5 [[1960 Valdivia earthquake]].
 
===Western margin===
{{Expand section|date=April 2013}}
==Intraplate features==
===Hotspots===
{{Main|Easter hotspot|Juan Fernández hotspot|Galápagos hotspot|San Felix hotspot}}
{{Expand section|date=December 2009}}
 
A second triple junction occurs at the northwest corner of the plate where the Nazca, Cocos, and Pacific Plates all join off the coast of [[Colombia]]. Yet another triple junction occurs at the southwest corner at the intersection of the Nazca, Pacific, and Antarctic Plates off the coast of southern [[Chile]]. At each of these triple junctions an ''[[:wikt:anomaly|anomalous]]'' microplate exists, the [[Galapagos Microplate]] at the northern junction and the [[Juan Fernandez Plate|Juan Fernandez Microplate]] at the southern junction. The [[Easter Plate|Easter Island Microplate]] is a third microplate that is located just north of the Juan Fernandez Microplate and lies just west of [[Easter Island]].
 
===Aseismic ridges===
{{Main|Nazca Ridge|Juan Fernández Ridge|Carnegie Ridge|}}
 
The '''Carnegie Ridge''' is a 1,350-km-long and up to 300-km-wide feature on the ocean floor of the northern Nazca Plate that includes the [[Galápagos Islands|Galápagos archipelago]] at its western end. It is being subducted under South America with the rest of the Nazca Plate.
 
===Fracture zones===
{{Empty section|date=March 2010}}
[[Darwin Gap]] is the area between the Nazca Plate and the coast of Chile, where [[Charles Darwin]] experienced the [[1835 Concepción earthquake|earthquake of 1835]]. It is expected that this area will be the epicenter of a major quake in the near future.<ref >Darwin Gap quake will shake Chile again [http://www.newscientist.com/article/dn20048-darwin-gap-quake-will-shake-chile-again.html], New Scientist, 30 Jan 2011, accessed 8 Feb 2011.</ref>
 
==Plate motion==
The absolute motion of the Nazca Plate has been calibrated at 3.7&nbsp;cm/yr east motion (88°), one of the fastest absolute motions of any tectonic plate. The subducting Nazca Plate, which exhibits unusual [[flat-slab subduction]], is tearing as well as deforming as it is subducted (Barzangi and Isacks). The subduction has formed, and continues to form, the [[volcano|volcanic]] [[Andes]] Mountain Range. Deformation of the Nazca Plate even affects the geography of [[Bolivia]], far to the east (Tinker et al.). It was on the Nazca Plate that the [[1994 Bolivia earthquake]] occurred; this had a magnitude of 8.2 <math>M_w</math> and was the strongest earthquake occurring deeper than 300&nbsp;km.
 
Luckily, besides the [[Juan Fernández Islands]], this area has very few islands to suffer the earthquakes that are a result of complicated movements at these junctions.
 
==Geologic history==
{{See also|Farallon Plate}}
 
The precursor of both the Nazca Plate and the [[Cocos Plate]] (to its north) was the [[Farallon Plate]], which split in late [[Oligocene]] times, about 22.8 [[mya (unit)|Mya]], a date arrived at by interpreting [[Geomagnetism|magnetic anomalies]].
 
==See also==
*[[1835 Concepción earthquake]]
*[[2010 Chile Earthquake]]
 
==References==
{{Reflist}}
 
;Bibliography
*[http://www.extremescience.com/PlateTectonicsmap.htm Extreme Science site: "A Lesson in Plate tetonics"] The basics explained.
*[http://www.earth.columbia.edu/news/2002/story12-05-02.html Galapagos rise junction (map)]
*[http://www.pmel.noaa.gov/vents/s-epr.html Juan Fernandez and Easter microplate (map)]
*Muawia Barazangi and Bryan L. Isacks, "Spatial distribution of earthquakes and subduction of the Nazca plate beneath South America" in ''Geology'' Vol. 4, No. 11, pp.&nbsp;686–692. [http://www.gsajournals.org/gsaonline/?request=get-abstract&doi=10.1130%2F0091-7613(1976)4%3C686:SDOEAS%3E2.0.CO%3B2 Abstract]
*Mark Andrew Tinker, Terry C. Wallace, Susan L. Beck, Stephen Myers, and Andrew Papanikolas, "Geometry and state of stress of the Nazca plate beneath Bolivia and its implication for the evolution of the Bolivian orocline" in ''Geology'' '''24'''(5), pp.&nbsp;387–390 [http://www.gsajournals.org/gsaonline/?request=get-abstract&doi=10.1130%2F0091-7613(1996)024%3C0387:GASOSO%3E2.3.CO%3B2 Abstract]
*Cahill, T. and B. Isacks (1992). "Seismicity and shape of the subducted Nazca plate." ''Journal Geophysical Research'' '''97''' (12)
*James, D. (1978). "Subduction of the Nazca plate beneath Central Peru." ''Geology'' '''6''' (3) pp 174 &ndash; 178
*[http://www-odp.tamu.edu/publications/170_SR/VOLUME/CHAPTERS/SR170_07.PDF Martin Meschede and Udo Barckhausen, "Plate tectonic evolution of the Cocos-Nazca spreading center"] (pdf file)
 
{{Tectonic plates}}
{{Central America plates}}
 
{{coord|14|49|44|S|74|56|37|W|region:PE_type:city(23000)_source:kolossus-ptwiki|display=title}}
 
[[Category:Tectonic plates]]
[[Category:Geology of Chile]]
[[Category:Natural history of South America]]
[[Category:Geology of the Pacific Ocean]]

Latest revision as of 00:37, 3 June 2014


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