Kōrero: Sea floor geology

New Zealand’s coastline in the ice age

New Zealand’s coastline in the ice age

In the last major glacial period some 20,000 years ago, New Zealand’s land area was much larger, as the sea was 120–30 metres lower than its present level. The three main islands were joined together as a single island. During this period, rivers such as the Clutha, Rakaia and Waimakariri carried huge loads of sediment all the way to the edge of the continental shelf. The Waikato River (dashed line) originally flowed north and entered the sea on the eastern side of the North Island. About 20,000 years ago it changed to its present course.

Te whakamahi i tēnei tūemi

Te Ara - The Encyclopedia of New Zealand

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Source: GNS Science

Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Te tuhi tohutoro mō tēnei whārangi:

Keith Lewis, Scott D. Nodder and Lionel Carter, 'Sea floor geology - The continental shelf', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/mi/map/5599/new-zealands-coastline-in-the-ice-age (accessed 8 December 2023)

He kōrero nā Keith Lewis, Scott D. Nodder and Lionel Carter, i tāngia i te 12 Jun 2006