Search results
Results from the WOW.Com Content Network
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.
Until about 18,000 years ago the Mataura drained Lake Wakatipu.The Kingston Flyer follows part of the former river bed, now blocked by glacial moraine. [2]For Māori, the Mataura was an important ara tawhito (traditional travel route) that provided direct access from Murihiku to Whakatipu Waimāori (Lake Wakatipu). [3]
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 Clarence River (Māori: Waiau Toa; officially Waiau Toa / Clarence River) is a major river which flows through the Kaikōura Ranges in the northeast of New Zealand's South Island. At roughly 209 kilometres (130 mi) long, it is the longest river in Canterbury and the eighth longest in New Zealand.
Using that boundary, Mackenzie Lakes had a population of 1,182 at the 2018 New Zealand census, an increase of 300 people (34.0%) since the 2013 census, and an increase of 399 people (51.0%) since the 2006 census. There were 375 households, comprising 585 males and 597 females, giving a sex ratio of 0.98 males per female.
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 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.
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.