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Vailuluʻu is a volcanic seamount discovered in 1975. It rises from the sea floor to a depth of 593 m (1,946 ft) and is located between Taʻu and Rose islands at the eastern end of the Samoa hotspot chain. The basaltic seamount is considered to mark the current location of the Samoa hotspot. The summit of Vailuluʻu contains a 2 km wide, 400 m deep…
History, Geography & Research
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seamount hydrothermal summit hotspot samoa crater nafanua volcanic volcano may ft ocean eruptions iron metres eruption cone located islands depth
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Vailuluʻu | Coordinates | .mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct,.mw-pars… | 1.00 | infobox |
| Vailuluʻu | Country | United States | 1.00 | infobox |
| Vailuluʻu | Discovery date | 1975 | 1.00 | infobox |
| Vailuluʻu | Height | 4,200 m (13,800 ft) | 1.00 | infobox |
| Vailuluʻu | Last eruption | 2003 | 1.00 | infobox |
| Vailuluʻu | Location | South Pacific Ocean | 1.00 | infobox |
| Vailuluʻu | Summit depth | 590 metres (1,940 ft) | 1.00 | infobox |
| Vailuluʻu | is a | conical seamount and reaches a depth of 593 metres | 0.90 | text |
| Fuji | instance of | and its height above the seafloor is comparable with that of major isolated volcanoes | 0.80 | text |
| although much smaller than compound volcanic islands such as Hawaii | instance of | and its height above the seafloor is comparable with that of major isolated volcanoes | 0.80 | text |
| Vailuluʻu | related to Biology | Various | 0.60 | section |
| Vailuluʻu | related to Biology | Tangaroa Seamount | 0.60 | section |
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