Tonga-Kermadec Ridge
The Tonga-Kermadec Ridge is an oceanic ridge in the south-west Pacific Ocean underlying the Tonga-Kermadec island arc.It is the most linear, fastest converging, and most seismically active subduction boundary on Earth, and consequently has the highest density of submarine volcanoes.
Havre Seamount
Hydrothermal vent
Kermadec Islands
Kermadec Trench
Lau Basin
Manihiki Plateau
Monowai (seamount)
North Fiji Basin
Tonga Trench
Vailuluʻu
Anarchias supremusCrocodile sharkGeology of New ZealandHelen BostockHikurangi PlateauKermadec-Tonga ArcKermadec-Tonga RidgeKermadec-Tonga subduction zoneKermadec ArcKermadec PlateKermadec RidgeLeptothyra kermadecensisOutline of oceanographyTonga ArcTonga RidgeTongaichthys robustusTosanoides flavofasciatus
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Tonga-Kermadec Ridge
The Tonga-Kermadec Ridge is an oceanic ridge in the south-west Pacific Ocean underlying the Tonga-Kermadec island arc.It is the most linear, fastest converging, and most seismically active subduction boundary on Earth, and consequently has the highest density of submarine volcanoes.
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The Tonga-Kermadec Ridge is an ...... IP has already been subducted.
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July 2018
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The Tonga-Kermadec Ridge is an ...... ensity of submarine volcanoes.
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Tonga-Kermadec Ridge
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