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Zelandija

Izvor: Wikipedija

Za ostale upotrebe, v. Zelandija (razvrstavanje).
Topografija Zelandije. Pravocrtne hrbate koji su u smjeru sjever-sjeveroistok i jugoistočno od Novog Zelanda ne smatra se dijelom mikrokontinenta, niti su Australijom (gore lijevo), Fidžijem niti Vanuatuima (u sredini na vrhu).[1]

Zelandija (engl. Zealandia), Tasmantis ili Novozelandski kontinent, naziv za potopljeni mikrokontinent koji se odlomio od Australije prije 60–85 milijuna godina, odnosno nakon što se australsko-zelandski kontinent odvojio od Antarktika prije 85–130 milijuna godina. Vjerojatno je potpuno potonuo oko 23 milijuna godina i danas je njegov najveći dio (93 %) pod Tihim oceanom, s iznimkom Novog Zelanda i Nove Kaledonije.

Vidi još

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  • kontinent
  • potkontinent
  • mikrokontinent
  • kontinentalni fragment
  • Zealandia Bank
  • Mauritia

Izvori

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  1. „Figure 8.1: New Zealand in relation to the Indo-Australian and Pacific Plates”. The State of New Zealand’s Environment 1997. 1997.. Pristupljeno 20. travnja 2007. 
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Zelandija
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