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1880s photos of Whatawhata Bridge, close up and 1924 rebuilding; 1907 photo of bridge at Ōtorohanga; Geological maps – 1925 Ngaruawahia, Whatawhata-Te Pahu, Pirongia, 1940 Ōtorohanga, upper Waipā and Pakaumanu. 1:50,000 map of source of Waipā River; Google street view images show several parts of the river, the uppermost being at Toa Bridge
The Rangitīkei River is one of New Zealand's longest rivers, 253 kilometres (157 mi) long. [2]Its headwaters are to the southeast of Lake Taupō in the Kaimanawa Ranges.It flows from the Central Plateau south past Taihape, Mangaweka, Hunterville, Marton, and Bulls, to the South Taranaki Bight at Tangimoana, 40 kilometres (25 mi) southeast of Whanganui.
The Manawatū is unique among New Zealand rivers in that it crosses a mountain range. The river has formed a "water gap" across the mountains because it is older than the Ruahine and Tararua Ranges. Most rivers arise from an already-existing range of mountains or hills, but beginning about 3 million years ago the central North Island mountain ...
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Before British colonisation of New Zealand, the Indigenous architecture of Māori was an 'elaborate tradition of timber architecture'. [1] Māori constructed rectangular buildings (whare) with a 'small door, an extension of the roof and walls to form a porch, and an interior with hearths along the centre and sleeping places along the walls' for protection against the cold.
The Hāpuku River begins in the Seaward Kaikōura Range of New Zealand and flows south-east to enter the South Pacific at Hapuka, between Clarence and Kaikōura. [1] The name comes from the Māori word hāpuku or hāpuka, a deep-water marine fish. [2] Its main tributary is the Puhi Puhi River.
New Zealand's lowest point, at 2m below sea level, is slightly north of the airport on Kirk's Drain Road, Momona. To the northeast, the city of Dunedin is separated from the Taieri Plain by a range of rugged hills which are part of the crater of an extinct volcano .
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