President Thiers Bank

{{short description|Broad guyot, northwest of Rapa, southeast of Raivavae, in the Austral Islands}}

{{Infobox seamount

|name=President Thiers Bank

|map=

|depth={{convert|33|m}}

|type=Guyot

|coordinates={{coord|24|40|S|145|55|W|display=inline,intitle|notes=}}

}}

President Thiers Bank is a broad guyot, which lies northwest of Rapa{{sfn|Maury|Guille|Guillou|Chauvel|2013|p=559}} and {{convert|200|km}} southeast of Raivavae,{{sfn|Maury|Guille|Guillou|Chauvel|2013|p=565}} in the Austral Islands.{{sfn|Maury|Guille|Guillou|Chauvel|2013|p=559}} Its summit reaches a depth of {{convert|33|m}}. It may have been created by the Macdonald hotspot. Another theory sees in the seamount the endpoint of an alignment that starts with Aitutaki{{sfn|Maury|Guille|Guillou|Chauvel|2013|p=558}} and also involves one volcanic phase at Raivavae.{{sfn|Maury|Guille|Guillou|Chauvel|2013|p=565}}

References

{{Reflist|refs=

{{cite journal|last1=Adam|first1=C.|last2=Bonneville|first2=A.|title=No thinning of the lithosphere beneath northern part of the Cook-Austral volcanic chains|journal=Journal of Geophysical Research|date=18 October 2008|volume=113|issue=B10|page=12|doi=10.1029/2007JB005313|url=https://hal-insu.archives-ouvertes.fr/insu-01288730/file/jgrb5313.pdf|bibcode=2008JGRB..11310104A}}

{{Cite book|title=World Regional Geology|last1=Fairbridge|first1=Rhodes W.|last2=Chevalier|first2=J.-P.|date=1975|publisher=Springer, Berlin, Heidelberg|isbn=978-3-540-31081-5|pages=499–500|language=en|doi=10.1007/3-540-31081-1_111}}

{{cite journal|last1=Menard|first1=H. W.|last2=McNutt|author-link2=Marcia McNutt|first2=Marcia|title=Evidence for and consequences of thermal rejuvenation|journal=Journal of Geophysical Research|date=1982|volume=87|issue=B10|page=8573|doi=10.1029/JB087iB10p08570|bibcode=1982JGR....87.8570M}}

{{cite journal|last1=Johnson|first1=Rockne H.|last2=Malahoff|first2=Alexander|title=Relation of Macdonald Volcano to migration of volcanism along the Austral Chain|journal=Journal of Geophysical Research|date=10 May 1971|volume=76|issue=14|page=3289|doi=10.1029/JB076i014p03282|bibcode=1971JGR....76.3282J}}

{{cite journal|last1=Bonneville|first1=Alain|last2=Suavé|first2=Raymond Le|last3=Audin|first3=Laurence|last4=Clouard|first4=Valérie|last5=Dosso|first5=Laure|last6=Gillot|first6=Pierre Yves|last7=Janney|first7=Philip|last8=Jordahl|first8=Kelsey|last9=Maamaatuaiahutapu|first9=Keitapu|title=Arago Seamount: The missing hotspot found in the Austral Islands|journal=Geology|date=1 November 2002|volume=30|issue=11|page=1025|doi=10.1130/0091-7613(2002)030<1023:ASTMHF>2.0.CO;2|language=en|issn=0091-7613|bibcode=2002Geo....30.1023B|s2cid=130183862}}

}}

= Sources =

{{refbegin}}

  • {{cite journal|last1=Maury|first1=R. C.|last2=Guille|first2=G.|last3=Guillou|first3=H.|last4=Chauvel|first4=C.|author-link4=Catherine Chauvel|last5=Rossi|first5=P.|last6=Pallares|first6=C.|last7=Legendre|first7=C.|title=Temporal evolution of a Polynesian hotspot: New evidence from Raivavae (Austral islands, South Pacific ocean)|journal=Bulletin de la Société Géologique de France|date=1 November 2013|volume=184|issue=6|pages=557–567|doi=10.2113/gssgfbull.184.6.557|language=en|issn=0037-9409}}

{{refend}}

Category:Seamounts of the Pacific Ocean

Category:Undersea banks of the Pacific Ocean

Category:Guyots

Category:Geography of the Austral Islands

Category:Citation overkill

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