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The Maori River is a river of the West Coast Region of New Zealand's South Island. It flows from several sources in the Mataketake Range east of Haast , passing through the small Tawharekiri Lakes before becoming a tributary of the Waita River , which flows into the Tasman Sea 15 kilometres north of Haast.
Land Information New Zealand – Search for Place Names; Booker, D.J.; Whitehead, A.L. (2017). "NZ River Maps: An interactive online tool for mapping predicted freshwater variables across New Zealand". niwa.co.nz. Christchurch: National Institute of Water and Atmospheric Research (NIWA). Young, David. "Rivers – Types of river.
The longest river in New Zealand is the Waikato River with a length of 425 kilometres (264 miles). The largest river by rate of flow is the Clutha River / Mata-Au with a mean discharge of 613 cubic metres per second (21,600 cu ft/s). [1] The shortest river is claimed to be the Tūranganui River in Gisborne at 1,200 metres (3,900 feet) long. [2]
The river was first known by its Māori name of Te Awa Whakatipu, with te awa literally translating as 'the river'. [7] The name Whakatipu is shared with several nearby geographic features, including Lake Wakatipu [a] and Whakatipu Kā Tuka (the Hollyford River) though this name is an archaic term and its original meaning is no longer known. [8]
The Pātea River is in Taranaki in the North Island of New Zealand. It runs for 105 kilometres from the eastern slopes of Mount Taranaki, passing east through Stratford before swinging south and reaching the South Taranaki Bight near the town of Patea. The river was the original portal to South Taranaki for both Māori and Europeans.
The Clutha River (Māori: Mata-Au, officially gazetted as Clutha River / Mata-Au) is the second longest river in New Zealand and the longest in the South Island.It flows south-southeast 338 kilometres (210 mi) through Central and South Otago from Lake Wānaka in the Southern Alps to the Pacific Ocean, 75 kilometres (47 mi) south west of Dunedin.
The Tutaekuri River (Māori: Tūtaekurī) flows eastward for 99.9 kilometres through the Hawke's Bay Region of the eastern North Island of New Zealand into the Pacific Ocean. It starts in the Kaweka Range roughly 50 kilometres north-east of Taihape , and reaches the sea just to the south of Napier , where the Ngaruroro and Clive Rivers join it.
The Wairoa River carries large quantities of fine sediment (clays, silts and sands) that cloaks both the bed and the banks of the river. The rate of sediment loss has increased because of changes in land use from native forest to pasture, and forestry and farming land use practices, with current sediment losses estimated to be approximately 240% higher than before human arrival.