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Waikato River

Longest river in New Zealand

  • 14 min read
  • 4 chapters
Waikato River
Unknown author · CC BY-SA 3.0

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The name Waikato comes from the Māori language and translates as flowing water. The Waikato River has spiritual meaning for various local Māori tribes, including the large Tainui, who regard it as a source of their mana, or pride. The widely respected marae of Tūrangawaewae is close to its banks at Ngāruawāhia.

For many years the Tainui tribe have sought to reestablish their links to the river after the New Zealand Wars (see Invasion of the Waikato) and the subsequent confiscations of the 1860s, and are continuing negotiations with the New Zealand government. The Tainui iwi was advised not to bring a case for the river before the Waitangi Tribunal as they would not win. An out-of-court settlement was arranged, and the deed of settlement signed by the Crown and Waikato-Tainui in August 2008 settled the raupatu claim to the Waikato River. However, other claims for land blocks and harbours are still outstanding. Waikato-Tainui now have joint management of the river with Waikato Regional Council.

Origin

The ancestral Waikato River flowed from an ancient lake (Lake Huka) in the centre of the North Island through deep gorges of welded ignimbrite and rhyolite, northward through the Hinuera Valley and Hauraki Basin into the Thames Estuary. It is possible that the river flowed through the Waikato Basin about a million years ago before returning to its Hinuera course. After the huge Oruanui eruption 27,000 years ago, ignimbrite was showered all over the North Island to a thickness of 200 metres (660 ft). A new lake was formed – Lake Taupō. The water accumulated until a new outlet was forced 120 metres (390 ft) above the present lake level, near Waihora Bay. Over the next few thousand years, the bed of the river was raised by large amounts of eruption debris. Then the original, blocked outlet suddenly gave way; the lake level fell 75 metres (246 ft) as about 80 cubic kilometres (19 mi3) of water and debris poured out in a catastrophic breakthrough flood, causing the river to change course near Piarere. The Hinuera Gap and Waitoa River are evidence of the river's former course. The water level dropped quickly, and the river stayed in this new course through the Maungatautari Gorge and Hamilton Basin. Deposits show that the Waikato River was already in the Waikato Basin 21,800 years ago.

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