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
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= 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:Geography of the Austral Islands
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