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 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 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.
The Taieri River (a misspelling of the original Māori name Taiari [1]) is the fourth-longest river in New Zealand and is in Otago in the South Island. [2] Rising in the Lammerlaw Range , it initially flows north, then east around the Rock and Pillar range before turning southeast, reaching the sea 30 kilometres (19 mi) south of Dunedin .
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 Whakatiki River joins the Hutt from the west and it is about this point the river starts to flow along the virtually straight Wellington geologic fault, which lies on the western side of the river valley. [5] At the lower end of the Upper Hutt floodplain is Taita Gorge, which separates Upper Hutt from Lower Hutt; this gorge is significantly ...
Like many important geographic features in New Zealand, the creation and exploration of Manawatū Gorge is an embedded part of traditional Māori history. According to tradition, the first Māori to discover the gorge was Whātonga, an explorer from the Kurahaupō canoe, who found the gorge in about the 12th century. [ 1 ]