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The Kermadec-Tonga subduction zone is a convergent plate boundary that stretches from the North Island of New Zealand northward. The formation of the Kermadec and Tonga Plates started about 4–5 million years ago. Today, the eastern boundary of the Tonga Plate is one of the fastest subduction zones, with a rate up to 24 cm/yr. The trench formed between the Kermadec-Tonga and Pacific Plates is also home to the second deepest trench in the world, at about 10,800 m, as well as the longest chain of submerged volcanoes.

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  • Kermadec-Tonga subdukzio eremua
  • Kermadec-Tonga subduction zone
  • Zona di subduzione delle Kermadec-Tonga
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  • Kermadec-Tonga subdukzio eremua plaka tektonikoen arteko muga konbergente bat da, Zeelanda Berriko Ipar Uhartetik iparralderantz dagoena. Subdukzio eremu horretan daude , Kermadeceko fosa eta Tongako fosa. Subdukzio eremu horretan, Pazifikoko plaka azpian subduzitzen ari da. Kermadec-Tonga subdukzio eremuak, hegoaldean, trantsizioa egiten du eskuineranzko albo mugimenduko urratze faila batera. Faila hori Ipar Uhartearen hegoaldean dago, eta deritzo.
  • The Kermadec-Tonga subduction zone is a convergent plate boundary that stretches from the North Island of New Zealand northward. The formation of the Kermadec and Tonga Plates started about 4–5 million years ago. Today, the eastern boundary of the Tonga Plate is one of the fastest subduction zones, with a rate up to 24 cm/yr. The trench formed between the Kermadec-Tonga and Pacific Plates is also home to the second deepest trench in the world, at about 10,800 m, as well as the longest chain of submerged volcanoes.
  • La zona di subduzione delle Kermadec-Tonga è una zona di subduzione situata nell'Oceano Pacifico, che si estende verdo nord a partire dall'Isola del Nord, in Nuova Zelanda, che rimane di poco a ovest di essa e include la fossa di Hikurangi, la fossa delle Kermadec e la fossa di Tonga.
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Kermadec_and_Tonga_Plates.jpg
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  • Kermadec-Tonga subdukzio eremua plaka tektonikoen arteko muga konbergente bat da, Zeelanda Berriko Ipar Uhartetik iparralderantz dagoena. Subdukzio eremu horretan daude , Kermadeceko fosa eta Tongako fosa. Subdukzio eremu horretan, Pazifikoko plaka azpian subduzitzen ari da. Kermadec-Tonga subdukzio eremuak, hegoaldean, trantsizioa egiten du eskuineranzko albo mugimenduko urratze faila batera. Faila hori Ipar Uhartearen hegoaldean dago, eta deritzo.
  • The Kermadec-Tonga subduction zone is a convergent plate boundary that stretches from the North Island of New Zealand northward. The formation of the Kermadec and Tonga Plates started about 4–5 million years ago. Today, the eastern boundary of the Tonga Plate is one of the fastest subduction zones, with a rate up to 24 cm/yr. The trench formed between the Kermadec-Tonga and Pacific Plates is also home to the second deepest trench in the world, at about 10,800 m, as well as the longest chain of submerged volcanoes.
  • La zona di subduzione delle Kermadec-Tonga è una zona di subduzione situata nell'Oceano Pacifico, che si estende verdo nord a partire dall'Isola del Nord, in Nuova Zelanda, che rimane di poco a ovest di essa e include la fossa di Hikurangi, la fossa delle Kermadec e la fossa di Tonga.
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