| Waitaki | |
|---|---|
 Lower Waitaki River pictured from the International Space Station | |
 The Waitaki River system | |
| Location | |
| Country | New Zealand |
| Region | Canterbury, Otago |
| District | Waimate, Waitaki |
| Cities | Otematata, Kurow, Duntroon, Glenavy |
| Physical characteristics | |
| Source | Southern Alps |
| • location | Lake Benmore, New Zealand |
| • coordinates | 44°21′S 170°12′E / 44.350°S 170.200°E |
| Source confluence | Ohau River and Tekapo Rivers |
| Mouth | Pacific Ocean |
• location | New Zealand |
• coordinates | 44°57′S 171°09′E / 44.950°S 171.150°E |
• elevation | 0 m (0 ft) |
| Length | 209 km (130 mi) |
| Discharge | |
| • location | Kurow |
| • average | 356 m3/s (12,600 cu ft/s) |
| Basin features | |
| Tributaries | |
| • left | Ahuriri, Otematata, Maerewhenua |
| • right | Hakataramea |
The Waitaki River is a large braided river in the South Island of New Zealand. It drains the Mackenzie Basin and runs 209 kilometres (130 mi) south-east to enter the Pacific Ocean between Timaru and Oamaru on the east coast. It starts at the confluence of the Ōhau and Tekapo rivers, now at the head of the artificial Lake Benmore, these rivers being fed by three large glacial lakes, Pukaki, Tekapo, and Ōhau at the base of the Southern Alps. The Waitaki flows through Lake Benmore, Lake Aviemore and Lake Waitaki, these lakes being contained by hydroelectric dams, Benmore Dam, Aviemore Dam and Waitaki Dam.[1] The Waitaki has several tributaries, notably the Ahuriri River and the Hakataramea River. It passes Kurow and Glenavy before entering the Pacific Ocean. The River lends its name the Waitaki District on the south side of the river bank.
The river's flow is normally low in winter, with flows increasing in spring when the snow cloaking the Southern Alps begins to melt, with flows throughout the summer being rainfall dependent and then declining in the autumn as the colder weather begins to freeze the smaller streams and streams which feed the catchment. The median flow of the Waitaki River at Kurow is 356 cubic metres per second (12,600 cu ft/s).[2]
The first major infrastructure improvements to the river were made between 1881 and 1914 with the construction of road and rail bridges at Kurow and Waitaki Bridge.
The middle of the river bed formed a traditional political boundary between Canterbury and Otago. The term "south of the Waitaki" is often used to refer to the Otago and Southland regions as one common area (the two regions share historical and ethnic relationships which make them distinct from the regions to the north of them).
The river is popular for recreational fishing and jetboating.
- ^ Waitaki River, An Encyclopaedia of New Zealand, edited by A. H. McLintock, originally published in 1966. Te Ara – The Encyclopedia of New Zealand, updated 26-Sep-2006.
- ^ Waitaki Catchment Hydrological Information, Table 3.2 Waitaki Catchment – Flow Statistics at Flow Recording Sites, February 2005, Ref. ME582, Ministry for the Environment website, retrieved 22 November 2007.