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The Waimakariri River is one of the largest rivers in Canterbury, on the eastern coast of New Zealand's South Island. It flows for 151 kilometres (94 mi) in a generally southeastward direction from the Southern Alps across the Canterbury Plains to the Pacific Ocean.
The Commonwealth Range is a north-south trending range of rugged mountains, 60 nautical miles long, located within the Queen Maud Mountains on the Dufek Coast of the continent of Antarctica. The range borders the eastern side of Beardmore Glacier from Keltie Glacier to the Ross Ice Shelf. The range is southeast of the Queen Alexandra Range, which is to the west of the Beardmore Glacier. It is west of the Hughes Range and north of the Supporters Range and the Barton Mountains.
The Conway River is part of the traditional boundary between the Canterbury and Marlborough regions in the South Island of New Zealand.
Crooked River is a river that flows from headwaters in the Southern Alps to Lake Brunner in the West Coast region of New Zealand's South Island. It is named for the erratic path it takes. Near Lake Brunner, it passes through reasonably flat farmland, but closer to its source, it rushes through gorges and rapids. One tributary is the Poerua River from Lake Poerua.
The Hinds River is a river in the Canterbury region of New Zealand. Its north and south branches drain the eastern flank of the Moorhouse Range, part of the Southern Alps, and their confluence is near Anama and Mayfield. The river then flows across the Canterbury Plains towards the Pacific Ocean, passing through the small town of Hinds along the way. In Hinds, State Highway 1 and the Main South Line railway cross the river. The river's mouth is located between the localities of Longbeach and Lowcliffe.
The Evans River is a short river in New Zealand's South Island. It arises near Mount O'Shanessy in the Kaimata Range of the Southern Alps and flows north-west and then south-west, joining the Crooked River several kilometres before the latter's outflow into Lake Brunner.
The Fleming River is a river of the eastern Catlins, New Zealand. A tributary of the Tautuku River, it rises west of Soaker Hill in the Maclennan Range and flows south-eastward through the Catlins Forest Park to join that river at Tautuku.
The Hangaroa River is a river in the Gisborne Region of New Zealand. Its source is the Huiarau Ranges in the Te Urewera National Park, and flows southeast to merge with the Ruakituri River near Te Reinga. The combined rivers form the Wairoa River, which flows south into Hawke Bay.
The Harman River is a river of New Zealand. It starts in the Browning Range of the Southern Alps and becomes the Arahura River, which flows into the Tasman Sea north of Hokitika.
The Haupiri River is a river of New Zealand. It starts near Mount Dixon in the Kaimata Range of the Southern Alps and flows north-west near to Lake Haupiri, then north-east to join the Ahaura River. The Ahaura joins the Grey River which flows into the Tasman Sea at Greymouth.
The Little Hohonu River is a river of New Zealand's West Coast Region. It flows northwest from its origins in the Hohonu Range southwest of Lake Brunner, reaching the Greenstone River / Hokonui 20 kilometres southeast of Greymouth.
The Orari River is a river of the south Canterbury region of New Zealand's South Island. It rises to the northwest of the Four Peaks Range, initially flowing north then east to circumnavigate the range before flowing southeast across the Canterbury Plains. It reaches the Pacific Ocean 8 kilometres (5 mi) east of Temuka. The towns of Geraldine and Orari are both close to its banks. The river has been identified as an Important Bird Area by BirdLife International because it supports breeding colonies of the endangered black-billed gull.
The Rough River, alternatively known as the Otututu River is a river of the West Coast Region of New Zealand's South Island. A major tributary of the Grey River, it flows south from its sources near Mount Uriah in the Paparoa Range 20 kilometres southeast of Charleston, to reach the Grey River to the southwest of the settlement of Ikamatua. The river is currently shown on maps as Otututu (Rough) River, although this orthography is no longer common for New Zealand Rivers.
The Toaroha River is a river of the West Coast Region of New Zealand's South Island. It flows generally north through a valley between the Toaroha and Diedrichs Ranges to reach the Kokatahi River 25 kilometres southeast of Hokitika.
The Waikiti River is a river of the West Coast Region of New Zealand's South Island. It flows generally north from it sources in the eastern Kaimata Range, roughly paralleling the course of its larger eastern neighbour, the Trent River. It reaches the Ahaura River 20 kilometres southeast of Lake Hochstetter.
Canterbury's Esk River is a tributary of the Waimakariri River. It rises in the Dampier Range near Esk Head, and flows southwest on the western side of the Puketeraki Range to reach the upper Waimakariri some 20 kilometres (12 mi) north of Springfield.
The Little Grey River, also known as the Māwheraiti is a river of the West Coast Region of New Zealand. It is a major tributary of the Grey River / Māwheranui which it joins at Ikamatua.
The Taipo River is a river of the central West Coast Region of New Zealand's South Island. It flows north from its sources west of Mount Rolleston, fed by the waters of several mountain streams. After some 15 kilometres it turns northeast to flow past the Bald Range before reaching the valley of the Taramakau River into which it flows 35 kilometres east of Hokitika.
The Hurunui River South Branch is a river in the Hurunui District of Canterbury, New Zealand.
The Greenstone River / Hokonui, also known as the Big Hohonu River, is a river on the West Coast of New Zealand's South Island. It rises in the Hohonu Range, an outlying range of the Southern Alps / Kā Tiritiri o te Moana, roughly 30 kilometres (19 mi) southeast of Greymouth. The river flows northwest for its entire length, eventually joining the same river valley as the larger Taramakau River near the town of Kumara. From here, the two rivers flow roughly parallel for around 5 kilometres (3.1 mi) before the Greenstone / Hokonui joins the Taramakau just shy of the latter's mouth in the Tasman Sea. The area surrounding the river was historically home to gold mining operations, following the discovery of payable amounts of gold in 1864. The township of Greenstone was established on the river in the wake of this discovery, with other industries including a sawmill soon being established.
References
- ↑ Peter Dowling, ed. (2004). Reed New Zealand Atlas. Reed Books. pp. map 69. ISBN 0-7900-0952-8.
- Land Information New Zealand - Search for Place Names
42°37′S171°25′E / 42.617°S 171.417°E