{{Short description|Small tectonic plate in the eastern Mediterranean Sea}} {{Infobox tectonic plate | image = File:AegeanPlate.png | alt = The Aegean plate | type = Micro | move_direction = south-west | move_speed = 37 mm/year | geo_features = Greece, Turkey, Aegean Sea }} thumb|290px

The '''Aegean Sea plate''' (also called the '''Hellenic plate''' or '''Aegean plate''') is a small tectonic plate located in the Eastern Mediterranean under Southern Greece and western Turkey. Its southern edge is the Hellenic subduction zone south of Crete, where the African plate is being swept under the Aegean Sea plate.<ref>Meier, T. ''et al.'' (2007) "A Model for the Hellenic Subduction Zone in the area of Crete based on seismological investigations" [https://books.google.com/books?id=rQ1mm4IzkAYC&pg=PA194 pp. 194–195] ''In'' Taymaz, Tuncay and Dilek, Yildirim (eds.) (2007) ''The Geodynamics of the Aegean and Anatolia'' Geological Society, London, pp. 183–200, {{ISBN|978-1-86239-239-7}}</ref> Its northern margin is a divergent boundary with the Eurasian plate.

The seafloor in this region is about 350 m below sea level, while the adjacent Black Sea and Mediterranean Sea are 1300&ndash;1500 m deep. For this reason it is considered a high plateau between the seas.<ref>{{Cite book|last=Sodoudi|first=Forough|url=https://nbn-resolving.org/urn:nbn:de:kobv:b103-05152|title=Lithospheric structure of the Aegean obtained from P and S receiver functions|date=2005|publisher=Potsdam Geoforschungszentrum Potsdam|oclc=179835425}}</ref> Evidence suggests the Aegean plate contains thinned continental crust, rather than oceanic crust. Since its creation the crust has been thinned through various processes, including post-orogenic collapse and crustal extension. This extension is responsible for the formation of the Gulf of Corinth.<ref name=":0" /><ref name=":1" />

Previous observations of the region's motion described the crust under the Aegean Sea as a part of the Anatolian plate, and the different directions of motion were explained as the plate rotating counterclockwise. Further measurements found that motion of the Aegean region differed from the previous model, so the two plates are now considered distinct from each other.<ref>{{Cite web|last=Simonelli|first=Glenn|title=Tectonics of the Aegean/Anatolian region|url=https://www.astro.indiana.edu/gsimonel/G554_paper.pdf|url-status=live|archive-url=https://web.archive.org/web/20200918232800/https://www.astro.indiana.edu/gsimonel/G554_paper.pdf|archive-date=2020-09-18}}</ref>

== Development == The Aegean Sea area is thought to be an actively extending back-arc region due to slab rollback on the Hellenic subduction zone.<ref name=":0">{{Cite journal|last1=Searle|first1=Michael P.|last2=Lamont|first2=Thomas N.|date=2020|title=Compressional origin of the Aegean Orogeny, Greece|journal=Geoscience Frontiers|volume=13 |issue=2 |page=101049|doi=10.1016/j.gsf.2020.07.008|s2cid=225356710 |doi-access=free}}</ref> This has resulted in extensive normal faulting and rifting, as well as the formation of a back-arc basin. This environment has created a number of horst and graben features on the seafloor, similar to basin and range topography. Many of the Aegean Islands are peaks from these features reaching above sea level.<ref>{{Cite encyclopedia|title=Basins and ranges|url=http://www.britannica.com/EBchecked/topic/585476/tectonic-basins-and-rift-valleys/49680/Basins-and-ranges|url-status=live|encyclopedia=Encyclopædia Britannica|archive-url=https://web.archive.org/web/20110312080846/http://www.britannica.com:80/EBchecked/topic/585476/tectonic-basins-and-rift-valleys/49680/Basins-and-ranges |archive-date=2011-03-12 }}</ref><ref>{{Cite book|last1=Higgins|first1=M. D.|url=https://www.researchgate.net/publication/257233658|title=A Geological Companion to Greece and the Aegean|last2=Higgins|first2=R.|publisher=Duckworth |location=London|year=1996|pages=16–25}}</ref> The southern part of the plate is 20–22&nbsp;km thick, while the northern part of the plate is 32–40&nbsp;km thick, which suggests that the extensional environment has only recently begun affecting the northern region.<ref name=":1">{{Cite journal|last1=Sodoudi|first1=F.|last2=Kind|first2=R.|last3=Hatzfeld|first3=D.|last4=Priestley|first4=K.|last5=Hanka|first5=W.|last6=Wylegalla|first6=K.|last7=Stavrakakis|first7=G.|last8=Vafidis|first8=A.|last9=Harjes|first9=H.-P.|last10=Bohnhoff|first10=M.|date=2006|title=Lithospheric structure of the Aegean obtained from P and S receiver functions|journal=Journal of Geophysical Research: Solid Earth|volume=111|issue=B12|doi=10.1029/2005JB003932|bibcode=2006JGRB..11112307S |issn=2156-2202|doi-access=free|hdl=11858/00-1735-0000-0001-3290-3|hdl-access=free}}</ref>

Prior to the extensional environment, the region underwent the Aegean Orogeny ({{Circa|70–14 Ma}}), followed by crustal thinning due to post-orogenic collapse. This period enabled metamorphism and then exhumation of many types of metamorphic rock found on the Aegean islands.<ref name=":0" />

== Seismic activity == The Aegean Sea and surrounding area is seismically active because of the Hellenic subduction zone, as well as the extension of the Aegean Plate. The African plate is subducting under the Aegean plate at a rate of about 40&nbsp;mm/year, causing shallow earthquakes near the fault and deeper earthquakes near the Greek volcanic arc.<ref>Herman, M.W., Hayes, G.P., Smoczyk, G.M., Turner, Rebecca, Turner, Bethan, Jenkins, Jennifer, Davies, Sian, Parker, Amy, Sinclair, Allison, Benz, H.M., Furlong, K.P., and Villaseñor, Antonio, 2015, Seismicity of the Earth 1900–2013, Mediterranean Sea and vicinity: U.S. Geological Survey Open-File Report 2010–1083-Q, scale 1:10,000,000, doi:[http://dx.doi.org/10.3133/ofr20101083Q 10.3133/ofr20101083Q].</ref> Some seismic activity is a result of the extension of the plate, which creates east–west trending faults that can slip and cause earthquakes.<ref>{{Citation|title=How did the 2020 Aegean Sea Earthquake happen? #utd gss #geonews|url=https://www.youtube.com/watch?v=MMBFY-LahNc|access-date=2021-12-02}}</ref>

==References== {{Reflist}}

==Further reading== *{{cite journal|last=Bird|first=P.|date=2003|title=An updated digital model of plate boundaries|journal=Geochemistry, Geophysics, Geosystems|volume=4|issue=3|pages=1027|url=http://peterbird.name/publications/2003_PB2002/2003_PB2002.htm|doi=10.1029/2001GC000252|bibcode=2003GGG.....4.1027B |citeseerx=10.1.1.695.1640|doi-access=free}} *{{Cite journal|last1=Müller|first1=R. Dietmar|last2=Zahirovic|first2=Sabin|last3=Williams|first3=Simon E.|last4=Cannon|first4=John|last5=Seton|first5=Maria|last6=Bower|first6=Dan J.|last7=Tetley|first7=Michael G.|last8=Heine|first8=Christian|last9=Breton|first9=Eline Le|last10=Liu|first10=Shaofeng|last11=Russell|first11=Samuel H. J.|date=2019|title=A Global plate Model Including Lithospheric Deformation Along Major Rifts and Orogens Since the Triassic|journal=Tectonics|volume=38|issue=6|pages=1884–1907|doi=10.1029/2018TC005462|bibcode=2019Tecto..38.1884M |s2cid=164552875 |issn=1944-9194|doi-access=free}}

==External links== {{commons category-inline}}

{{Tectonic plates}} {{Geology of Europe}} {{Authority control}}

Category:Tectonic plates Category:Aegean Sea Category:Geology of Greece Category:Geology of Turkey