President Thiers Bank is a broad[2]guyot,[3] which lies northwest of Rapa[4] and 200 kilometres (120 mi) southeast of Raivavae,[5] in the Austral Islands.[4] Its summit reaches a depth of 33 metres (108 ft).[6] It may have been created by the Macdonald hotspot.[7] Another theory sees in the seamount the endpoint of an alignment that starts with Aitutaki[8] and also involves one volcanic phase at Raivavae.[5]
^Johnson, Rockne H.; Malahoff, Alexander (10 May 1971). "Relation of Macdonald Volcano to migration of volcanism along the Austral Chain". Journal of Geophysical Research. 76 (14): 3289. Bibcode:1971JGR....76.3282J. doi:10.1029/JB076i014p03282.
Maury, R. C.; Guille, G.; Guillou, H.; Chauvel, C.; Rossi, P.; Pallares, C.; Legendre, C. (1 November 2013). "Temporal evolution of a Polynesian hotspot: New evidence from Raivavae (Austral islands, South Pacific ocean)". Bulletin de la Société Géologique de France. 184 (6): 557–567. doi:10.2113/gssgfbull.184.6.557. ISSN0037-9409.