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Sediments of the New Zealand Geosyncline form the oldest rocks in the North Island.

The zones in New Zealand are defined by trenches in the north and in the south and by the Alpine Fault which connects the two.

About 85 million years ago a rift valley formed to separate the New Zealand region from the rest of Gondwana, resulting in the formation of a new ocean floor by means of and by the Oligocene period (about 35 million years ago) most of the country was submerged.

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.

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