what continent is new zealand part of map
Zealandia Zealandia ( /ziːˈlændiə/), also known as the New Zealand continent or Tasmantis,[2] is a nearly submerged mass of continental crust that sank after breaking away from Australia 60–85 million years ago, having separated from Antarctica between 85 and 130 million years ago.[3] It has variously been described as a continental fragment, a microcontinent and a continent.[4] The name and concept for Zealandia were proposed by Bruce Luyendyk in 1995.[5]
History of New Zealand From 1840 there was considerable European settlement, primarily from England and Wales, Scotland and Ireland; and to a lesser extent the United States, India, China, and various parts of continental Europe, including the province of Dalmatia[59] in what is now Croatia, and Bohemia[60] in what is now the Czech Republic. Already a majority of the population by 1859, the number of Pākehā settlers increased rapidly to reach over one million by 1916.[61]