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Widespread tectonic activity continued from 10 million years ago to the modern, and during this time the principal mountain ranges of both islands were uplifted and New Zealand began taking its modern shape. The subduction of the Pacific plate caused much volcanism in the North Island, starting initially in Northland in the early Miocene and moving south over time until it reached its present position along the Taupo Volcanic Zone. Your News is the place for you to save content to read later from any device.Register with us and content you save will appear here so you can access them to read later.
At the end of this period a new rift valley formed between Australia and Antarctica and the sea floor spreading still continues. The Kaikoura Orogeny, Miocene to Quaternary period (24 million years ago to modern) Due to the new spreading ridge between Antarctica and Australia there was a build up of strain in the southwest Pacific crust that led to vertical and transcurrent fault movements.
The Torlesse supergroup rocks were deposited further away from a landmass, mostly in deep water, and the Murihiku rocks represent mainly 4.
The Rangitata Orogeny, Early Cretaceous period (about 142 to 99 million years ago) During this orogeny, the previously deposited geosyncline (3) sediments were compressed and folded.
Reference Websites Find out more about New Zealand's volcanoes on: Books Nelson C.
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