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Rangitoto Island

Rangitoto Island is a volcanic island in the Hauraki Gulf near Auckland, New Zealand. It has become an icon of Auckland as its distinctive symmetrical cone is visible from much of the city. It is the most recent and the largest of the approximately 48 volcanoes of the Auckland Volcanic Field. It was formed by a series of eruptions that ended about 500 years ago. It is not expected to erupt again although fresh eruptions are likely elsewhere in the Auckland Volcanic Field.


Rangitoto Island as viewed from North Head

The full name of Rangitoto Island is Nga Rangi-i-totongia-a Tama-te-kapua ('the days of the bleeding of Tama-te-kapua'). Tama-te-kapua was the captain of the Arawa canoe and was badly wounded on the island.

There are daily ferry trips to the island from Auckland but staying overnight is prohibited. Thirty years ago, there were houses perched on the island's edge in a ring, but as these became uninhabited they were removed. A day trip allows a good walk to the summit, with stunning views of the harbour and city.

There are no streams on the island so plants grow using only rainfall, yet the island is tree covered and also offers the chance to view some more unusual plants such as the kidney fern [1]. It has a large forest of naturally cross-bred pohutukawa and rata trees. Introduced brushtail possums and wallabies were eradicated in the late 20th century.

It is linked by a causeway to the much older, non-volcanic island of Motutapu, where it is possible to view the archeological remains of a civilisation caught in Rangitoto's eruptions.

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