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Vailuluʻu
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Vailuluʻu is a volcanic seamount discovered in 1975. It rises from the sea floor to a depth of 593 m and is located between Taʻu and Rose islands at the eastern end of the Samoa hotspot chain. The bas
The summit of Nafanua is covered with thick microbial mats, indicative of low-temperature venting
The summit of Nafanua is covered with thick microbial mats, indicative of low-temperature venting
Broken pillow lavas, colored red by iron oxide, inside Vailuluʻu crater.
Broken pillow lavas, colored red by iron oxide, inside Vailuluʻu crater.
An octopus living on the western summit of Vailulʻu
An octopus living on the western summit of Vailulʻu
Swimming elasipod sea cucumber, Paleopatides sp., photographed off the northern shore of Tau Island, Vailuluʻu Expedition 2005
Swimming elasipod sea cucumber, Paleopatides sp., photographed off the northern shore of Tau Island, Vailuluʻu Expedition 2005
Tonga–Kermadec Ridge
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The Tonga–Kermadec Ridge is an oceanic ridge in the south-west Pacific Ocean underlying the Tonga–Kermadec island arc. It is a result of the most linear, fastest converging, and seismically active sub
The Tonga–Kermadec Ridge runs along the Tonga–Kermadec Trench or subduction zone.
The Tonga–Kermadec Ridge runs along the Tonga–Kermadec Trench or subduction zone.