Peru–Chile Trench

{{Short description|Oceanic trench in the Pacific Ocean off South America}}

{{more citations needed|date=September 2014}}

Image:Peru-Chile trench.jpg

The Peru–Chile Trench, also known as the Atacama Trench, is an oceanic trench in the eastern Pacific Ocean, about {{convert|160.|km}} off the coast of Peru and Chile.{{cite encyclopedia|title=Peru-Chile Trench|url=http://www.britannica.com/EBchecked/topic/453259/Peru-Chile-Trench|encyclopedia=Encyclopædia Britannica|access-date=April 21, 2014}} It reaches a maximum depth of {{Convert|8065|m|ft|abbr=on}} below sea level in Richards Deep ({{Coord|23|10|45|S|71|18|41|W|display=inline}}) and is approximately {{Convert|5900.|km|mi|abbr=on}} long; its mean width is {{Convert|64|km|mi|abbr=on}} and it covers an expanse of some {{Convert|590000|km2|mi2|abbr=on}}.

The trench delineates the boundary between the subducting Nazca plate and the overriding South American plate.

Geology

The trench is a result of a convergent plate boundary, where the eastern edge of the oceanic Nazca plate is being subducted beneath the continental South American plate. The trench is also a part of the Chile triple junction, an unusual junction that consists of a mid-oceanic ridge and the Chile Rise being subducted under the South American plate at the Peru–Chile Trench. Two seamount ridges within the Nazca plate enter the subduction zone along this trench: the Nazca Ridge and the Juan Fernández Ridge.

From the Chile triple junction to Juan Fernández Ridge the trench is filled with {{convert|2.0|–|2.5|km}} of sediments, creating a flat bottom topography. Sediments are mainly turbidites interspersed with oceanic deposits of clay, volcanic ash, and siliceous ooze.

The Peru–Chile Trench, the forearc and the western edge of the central Andean plateau (Altiplano), delineate the dramatic "Bolivian Orocline" that defines the Andean slope of southern Peru, northern Chile, and Bolivia.

Oceanography

Most of the time, the trade winds drive surface waters offshore near the equator, driving the Humboldt Current from the tip of southern Chile to northern Peru. This current is associated with upwelling of deep, nutrient-rich water off the coast of Peru.{{cite web|title=Peru-Chile Trench|url=http://oceana.org/en/explore/marine-places/peru-chile-trench|work=Oceana|access-date=April 21, 2014|url-status=dead|archive-url=https://web.archive.org/web/20140825094639/http://oceana.org/en/explore/marine-places/peru-chile-trench|archive-date=August 25, 2014}} At times, El Niño disrupts the usual wind pattern and lessens the upwelling. The consequent loss of nutrient causes fish kills.

Biology

In 2018, three new species of snailfish were discovered thriving in the depths of the Atacama Trench.Wang, Amy, Scientists discover three new sea creatures in depths of the Pacific Ocean, The Washington Post, Wednesday, September 12, 2018{{cite web|url=https://www.theguardian.com/environment/2018/sep/15/gel-like-see-through-fish-discovered-75km-down-on-pacific-ocean-floor|title='Gel-like' see-through fish discovered 7.5 km down on Pacific ocean floor|work=The Guardian|date=2018-09-15}}

In 2023, a predatory crustacean was discovered in the Atacama Trench.{{Cite web |last=Dixit |first=Mrigakshi |title=Atacama Trench's terrifying new resident survives at 25,900 feet |url=https://interestingengineering.com/science/atacama-trenchs-new-resident-at-25900-feet |access-date=2024-12-23 |website=Interesting Engineering |language=en}}

Associated seismicity

File:USGS AmSo 0120170002fig1.png

File:USGS AmSo 0120170002fig11a.png

The subduction of the Nazca plate below the South American plate along the Chile-Peru Trench is associated with numerous earthquakes. Several of these earthquakes are notable for their size, associated tsunamis, and landslides.

See also

References

{{reflist}}

Further reading

  • {{Cite journal |last=Graham |first=Alan |date=2009-09-28 |title=The Andes: A Geological Overview from a Biological Perspective |url=http://dx.doi.org/10.3417/2007146 |journal=Annals of the Missouri Botanical Garden |volume=96 |issue=3 |pages=371–385 |doi=10.3417/2007146 |issn=0026-6493}}
  • {{Cite journal |last1=Mofjeld |first1=Harold |last2=Symons |first2=Christina |last3=Lonsdale |first3=Peter |last4=González |first4=Frank |last5=Titov |first5=Vasily |date=2004-03-01 |title=Tsunami Scattering and Earthquake Faults in the Deep Pacific Ocean |url=http://dx.doi.org/10.5670/oceanog.2004.65 |journal=Oceanography |volume=17 |issue=1 |pages=38–46 |doi=10.5670/oceanog.2004.65 |issn=1042-8275|doi-access=free }}
  • {{Cite journal|last1=Fisher |first1=Robert L. |last2=Raitt |first2=Russell W. |date=1962|title=Topography and structure of the Peru-Chile trench |url=http://dx.doi.org/10.1016/0011-7471(62)90094-3 |journal=Deep Sea Research and Oceanographic Abstracts |volume=9 |issue=11–12 |pages=423–443 |doi=10.1016/0011-7471(62)90094-3 |issn=0011-7471|url-access=subscription }}
  • {{Cite journal |last1=Wortel |first1=M.J.R. |last2=Cloetingh |first2=S.A.P.L. |date=1985 |title=Accretion and lateral variations in tectonic structure along the Peru-Chile Trench |url=http://dx.doi.org/10.1016/0040-1951(85)90190-8 |journal=Tectonophysics |volume=112 |issue=1–4 |pages=443–462 |doi=10.1016/0040-1951(85)90190-8 |issn=0040-1951|hdl=1871/8418 |hdl-access=free }}

{{geology of Chile}}

{{2010 Chile earthquake}}

{{coord|23|S|71|W|type:waterbody_source:dewiki|display=title}}

{{DEFAULTSORT:Peru-Chile Trench}}

Category:Geology of Chile

Category:Geology of Peru

Category:Landforms of Chile

Category:Landforms of Peru

Category:Lowest points of the World Ocean

Category:Natural history of South America

Category:Oceanic trenches of the Pacific Ocean

Category:Subduction zones