Auckland (Tāmaki-makau-rau)

In Māori Auckland’s name is Tāmaki-makau-rau, or the transliterated version of Auckland, Ākarana.

Auckland lies between the Hauraki Gulf of the Pacific Ocean to the east, the low Hunua Ranges to the south-east, the Manukau Harbour to the south-west, and the Waitakere Ranges and smaller ranges to the west and north-west. The central part of the urban area occupies a narrow isthmus between the Manukau Harbour on the Tasman Sea and the Waitemata Harbour on the Pacific Ocean. It is one of the few cities in the world to have harbours on two separate major bodies of water.

The isthmus was first settled around 1350 and was valued for its rich and fertile land. Many pā (fortified villages) were created, mainly on the volcanic peaks. Māori population in the area is estimated at about 20,000 people before the arrival of Europeans. The subsequent introduction of firearms, which began in Northland, upset the balance of power and led to devastating inter-tribal warfare, causing iwi who lacked the new weapons to seek refuge in areas less exposed to coastal raids. As a result, the region had relatively low numbers of Māori when European settlement of New Zealand began.  Joseph Brooks Weller, eldest of the Weller brothers of Otago and Sydney bought land including the sites of the modern cities of Auckland and North Shore and part of Rodney District, for “one large cask of powder” from “Cohi Rangatira”.

Volcanoes

Auckland straddles the Auckland Volcanic Field, which has produced approximately 50 volcanoes. These take the form of cones, lakes, lagoons, islands and depressions, and several have produced extensive lava flows. The individual volcanoes are all considered extinct, although the volcanic field itself is merely dormant.

Unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taupo, Auckland’s volcanoes are fueled entirely by basaltic magma. The most recent and by far the largest volcano, Rangitoto Island, was formed within the last 1000 years, and its eruptions destroyed the Māori settlements on neighbouring Motutapu Island some 700 years ago. Rangitoto’s size, its symmetry, its position guarding the entrance to Waitemata Harbour and its visibility from many parts of the Auckland region make it Auckland’s most iconic natural feature. Few birds and insects inhabit the island because of the rich acidic soil and the type of flora growing out of the rocky soil.