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Whanganui River

Coordinates: 39°56.89′S 174°59.22′E / 39.94817°S 174.98700°E / -39.94817; 174.98700
From Wikipedia, the free encyclopedia

Whanganui River
The Whanganui River. Mount Ruapehu can partly be seen at the top right of the scene.
The Whanganui River system
Native nameWhanganui (Māori)
Location
CountryNew Zealand
RegionManawatū-Whanganui
Towns and citiesTaumarunui, Whanganui
Physical characteristics
SourceMount Tongariro
MouthTasman Sea
 • coordinates
39°56.89′S 174°59.22′E / 39.94817°S 174.98700°E / -39.94817; 174.98700
 • elevation
Sea level
Length290 km (180 mi)
Basin size7,380 km2 (2,850 sq mi)
Discharge 
 • average219 m3/s (7,700 cu ft/s)[1]
Basin features
Tributaries 
 • leftWhakapapa River, Retaruke River, Manganui o te Ao River
 • rightPungapunga River, Ongarue River, Ohura River, Tangarakau River, Whangamōmona River

The Whanganui River is a major river in the North Island of New Zealand. It is the country's third-longest river, and has special status owing to its importance to the region's Māori people. In March 2017 it became the world's second natural resource (after Te Urewera) to be given its own legal identity, with the rights, duties and liabilities of a legal person. The Whanganui Treaty settlement brought the longest-running litigation in New Zealand history to an end.[2][3]

Geography

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With a length of 290 kilometres (180 mi), the Whanganui is the country's third-longest river. Much of the land to either side of the upper reaches is part of the Whanganui National Park, though the river itself is not part of the park.

The river rises on the northern slopes of Mount Tongariro, one of the three active volcanoes of the central plateau, close to Lake Rotoaira. It flows to the north-west before turning south-west at Taumarunui. From here it runs through the rough, bush-clad hill country of the King Country before turning south-east and flowing past the small settlements of Pipiriki and Jerusalem, before reaching the coast at the city of Whanganui. It is one of the country's longest navigable rivers.[4]

The river valley changed in the 1843 Wanganui earthquake.

In 1975, a minor eruption from Mount Ruapehu spilled some of the contents from the Ruapehu Crater Lake (the same root cause of the Tangiwai disaster). This toxic water entered the Whanganui River and had the effect of killing much of the fish life downstream. In the aftermath of the poisoning, eels as large as 8.2 kilograms (18 lb) and trout as large as 2.3 kilograms (5.1 lb) were washed up dead along the banks of the river.[5] The tributary Whakapapa River had fish losses due to a lahar from Ruapehu in April 1975.[6] Possibly this had effects downstream.

Tributaries

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Tributary name Length (km) Km from mouth Confluence coordinates Altitude
Mount Tongariro River source 290 km 39°07.91′S 175°37.95′E / 39.13183°S 175.63250°E / -39.13183; 175.63250
Whakapapa River 65 km (40 mi) 38°55′48″S 175°24′28″E / 38.93000°S 175.40778°E / -38.93000; 175.40778 255 m (837 ft)
Pungapunga River 22 km (14 mi) 38°53′30″S 175°20′0″E / 38.89167°S 175.33333°E / -38.89167; 175.33333 172 m (564 ft)
Ongarue River 73 km (45 mi) 38°53′31″S 175°15′11″E / 38.89194°S 175.25306°E / -38.89194; 175.25306 144 m (472 ft)
Ōhura River 134 km (83 mi) 39°02′20″S 175°3′52″E / 39.03889°S 175.06444°E / -39.03889; 175.06444 114 m (374 ft)
Retaruke River 64 km (40 mi) 39°06′9″S 175°4′12″E / 39.10250°S 175.07000°E / -39.10250; 175.07000 108 m (354 ft)
Tangarakau River 26 km (16 mi) 39°14′17″S 174°52′52″E / 39.23806°S 174.88111°E / -39.23806; 174.88111 85 m (279 ft)
Whangamōmona River 22 km (14 mi) 39°16′17″S 174°53′23″E / 39.27139°S 174.88972°E / -39.27139; 174.88972 82 m (269 ft)
Manganui o te Ao River 32 km (20 mi) 39°24′18″S 175°2′42″E / 39.40500°S 175.04500°E / -39.40500; 175.04500 62 m (203 ft)
Tasman Sea River mouth 0 km 39°56.89′S 174°59.22′E / 39.94817°S 174.98700°E / -39.94817; 174.98700 0 m

History

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Kawana flour mill, 1854 (restored), Matahiwi

Māori legend explains the formation of the river in the Mount Taranaki legend. When Mount Taranaki left the central plateau for the coast, the land was split open, and the river filled the rift.

Another Māori legend explains that after Māui caught the giant fish that was to become the North Island of New Zealand, known as Te Ika-a-Māui, he prayed to Ranginui who then sent two tear drops to land on Māui's fish. These two tear drops then became the rivers Whanganui and Waikato.

According to Māori tradition, the river was first explored by Tamatea, one of the leaders of the original migration to the new land, who travelled up the river and on to Lake Taupō. Many places along the river are named in his honour.

The Whanganui River was an important communication route to the central North Island, both for Māori and for settlers, despite many stretches of white water and over 200 rapids. Prior to the arrival of Europeans, the area around the Whanganui was densely inhabited and with the arrival of the colonial settlers, the area near the river's mouth became a major trading post.

Although it was already a significant route to the interior, the major development of the river as a trade route was by Alexander Hatrick, who started the first regular steam-boat service in 1892. The service eventually ran to Taumarunui where rail and coach services connected with points north. One of Hatrick's original boats, paddle-steamer PS Waimarie, has been restored and runs scheduled sailings in Whanganui. Another of the Hatrick boats, MV Wairua, has also been restored and can be seen on the river.

During the early 20th century, the Wanganui River, as it was then called, was one of the country's top tourist attractions, its rugged beauty and the Māori kāinga (villages) that dotted the banks attracting thousands of tourists a year.

With the completion of the North Island Main Trunk railway, the need for the steamboat route to the north greatly diminished, and the main economic activity of the river area became forestry. During the 1930s, attempts were made to open the river valley up as farmland, but they were not successful. One legacy of that time is the Bridge to Nowhere, built to provide access to settlements long since abandoned.

In 1912–13 the French filmmaker Gaston Méliès shot a (now lost) documentary film The River Wanganui about the river, calling it the Rhine of New Zealand.

The settlement of Jerusalem is of particular note. Jerusalem was home to two famous New Zealanders, Mother Mary Joseph Aubert, whose Catholic mission is still located at Jerusalem, and New Zealand poet James K. Baxter, who established a commune at the settlement in 1970.

Other settlements are Tieke Kāinga, Pipiriki, Rānana, Matahiwi, and Koriniti.

Taonga and Māori land claims

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The river is of special and spiritual importance for Māori, who also refer to it as Te awa tupua. It was the home for a large proportion of Māori villages in pre-European times. As such, it is regarded as taonga, a special treasure. Local iwi first petitioned Parliament in the 1870s,[7] and efforts have since been made to safeguard the river and give it the respect it deserves.

For the same reason, the river has been one of the most fiercely contested regions of the country in claims before the Waitangi Tribunal for the return of tribal lands. The Whanganui River claim is heralded as the longest-running legal case in New Zealand history[8] with petitions and court action in the 1930s, Waitangi Tribunal hearings in the 1990s, the ongoing Tieke Marae land occupation since 1993, and the highly publicised Moutoa Gardens occupation in 1995.[9]

On 30 August 2012 agreement was reached that entitled the Whanganui River to a legal identity,[10] a first in the world,[7] and on 15 March 2017 the relevant settlement was passed into law (Te Awa Tupua (Whanganui River Claims Settlement) Act 2017) by the New Zealand Parliament.[11] Chris Finlayson, the Minister for Treaty of Waitangi Negotiations, said the river would have an identity "with all the corresponding rights, duties and liabilities of a legal person". He said some people would consider it strange, but it is "no stranger than family trusts, or companies, or incorporated societies."[12][13] The bill finalised 140-year-old negotiations between Māori and the government.[3] The river will be represented by two officials, one from Māori and the other from the government.[2]

Naming

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Whanga nui is a phrase meaning "big bay"[14] or "big harbour". Some very early maps show that European settlers called the river the Knowsley River,[15] however it was known as the Wanganui River until its name was officially changed to Whanganui in 1991,[16] respecting the wishes of local iwi. Part of the reason for this change was also to avoid confusion with the Wanganui River in the South Island. The city at the river's mouth was called Wanganui until December 2009, when the government decided that while either spelling was acceptable, Crown agencies would use the Whanganui spelling.[17]

See Controversy over Wanganui/Whanganui spelling

Fauna and flora

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Blue duck (whio) at Staglands, Akatarawa, New Zealand

Native fish species in the river include Cran's bully, upland bully, climbing galaxias (kōaro), longfin and short-finned eels, pouched lamprey, shortjaw kokopu, torrentfish, New Zealand smelt[18] and black flounder.[19] Introduced brown and rainbow trout are found, although not in high numbers, and there have been reports of catfish.[18]

Other native aquatic species include koura[19] and declining numbers of New Zealand freshwater mussels.[20] The river and its tributaries are home to a variety of invertebrates such as mayflies, stoneflies and caddis flies.[18]

Blue duck (whio) populations can be found at the junction of the Whanganui River and the Mangatepopo and Okupata streams.[21] The Nankeen night heron established roosts along the Whanganui River in the 1990s and is breeding in New Zealand only in this location.[22]

Much of the flora in the river basin can be characterised as a broadleaf and podocarp forest;[23] understory species include crown fern (Blechnum discolor), and a variety of other ferns and shrubs.[24]

River boats

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In 1892 Alexander Hatrick was contracted by Thomas Cook & Son to carry tourists to Pipiriki[25] on the paddle-steamer PS Waimarie, the journey was "The Rhine of Maoriland" tourist route into the interior of New Zealand. The river boat subsequently carried mail, passengers and cargo.

PS Waimarie operates on the lower stretches of the river, including dinner cruises to Avoca Hotel at Upokongaro and trips to Hipango Park for overnight camping.[26]

On 18 June 2010 the Adventurer 2 river boat embarked,[27] attempting to make the 230-kilometre (140 mi) voyage to Taumarunui. The first voyage to Taumarunui in 82 years. The Adventurer 2 now offers this trip to tourist as an historic alternative to jet boating and canoeing the river.[28] Though in low water flows it cannot make it all the way to Taumarunui.

River boat landings

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One of the many Māori marae along the Whanganui River

The Whanganui River was the supply artery for the early communities along its banks. River boats used to ply the river, and also into the Ohura River and Ongarue Rivers unless these routes were log jammed after floods.

Between 1891 and 1958 the Alexander Hatrick Riverboat service operated on the Whanganui River. The paddle-steamer Wairere ordered from London and shipped in sections then assembled in Whanganui in late 1891.

It is said that Taumarunui was the highest reach of the Whanganui River that was navigable by river boat. The river flow was managed by the "Wanganui River Trust Board" which built containing walls to direct and deepen the rivers channels for river traffic. Even so, river boats sometimes found it necessary to winch themselves up the more difficult rapids. The River Trust existed from 1891 to 1940.[29]

Landing name Community serviced Distance from mouth Travel time up/down Coordinates
Taumarunui Landing Taumarunui 144 mi (232 km)[30]
Kirikau Landing Kirikau
Te Maire Landing Te Maire
Otumangu Landing Otumangu 132 mi (212 km)[30]
Lacy's Landing
Wades Landing Retaruke Valley 108 mi (174 km)[31] 39°6.65′S 175°3.98′E / 39.11083°S 175.06633°E / -39.11083; 175.06633
Mangapurua Landing Mangapurua Valley 75 mi (121 km)[32]
Tangahoe Landing Tangahoe 73 mi (117 km)[32]
Mangatiti Landing Mangatiti 72 mi (116 km)[32]
Parinui Landing Parinui 71 mi (114 km)[32]
Ramanui Landing Ramanui 70 mi (110 km)[32]
Pipiriki landing Pipiriki
Lower Pipiriki landing Pipiriki 57 mi (92 km)[32]
Te Tuhi Landing Ahuahu Stream valley
Hipango Park Landing ?
Up-river Landing
Wanganui Wharves Whanganui

Recreational use

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Kayaking is a very popular sport on the river.

The flow of the river has been altered with the diversion of water from the headwaters by the Tongariro Power Scheme and into Lake Taupō. This may have been a contributing factor to the demise of the raft race and means river boats can no longer make the entire trip to Taumarunui during the drier months (see below).

Bridges

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Despite being New Zealand's longest navigable river, the Whanganui has few bridges. Only two are located on the 230-kilometre (140 mi) stretch between Whanganui and Taumarunui. The complete list of bridges in order from source to sea are:

Whanganui –

A bridge over the Whanganui to connect Raetihi to Taranaki was to be constructed in the Mangaparua area (where the Bridge to Nowhere) is located, but this plan was never implemented.

Rail bridges

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The oldest bridges over the river are rail bridges; the Aramoho Rail Bridge of 1876 in Whanganui and the Matapuna Bridge of 1903-1904 near Taumarunui.[39]

Notable people

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References

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  1. ^ "NIWA Water & soil miscellaneous publication no. 48 (1983)" (PDF). docs.niwa.co.nz. Retrieved 5 March 2023.
  2. ^ a b Davison, Isaac. "Whanganui River given legal status of a person under unique Treaty of Waitangi settlement". The New Zealand Herald. Retrieved 16 March 2017.
  3. ^ a b Roy, Eleanor Ainge (16 March 2017). "New Zealand river granted same legal rights as human being". The Guardian. London, United Kingdom. Retrieved 16 March 2017.
  4. ^ "Manawatu and Whanganui Region". Jasons Travel Media.
  5. ^ "Ruapehu throws up more ash". The Press. 28 April 1975. p. 1 – via Papers Past.
  6. ^ J. Richardson; L. D. Teirney (October 1982). "The Whakapapa River: A Study of a Trout Fishery" (PDF). NIWA. Retrieved 5 March 2023.
  7. ^ a b "Innovative bill protects Whanganui River with legal personhood". www.parliament.nz. 28 March 2017. Retrieved 3 September 2022.
  8. ^ "Whanganui Tribes". teara.govt.nz. Retrieved 5 March 2023.
  9. ^ See also Moutoa Island
  10. ^ "Whanganui Iwi (Whanganui River) Deed of Settlement Summary". New Zealand Government. 17 November 2020. Retrieved 3 September 2022.
  11. ^ "Te Awa Tupua (Whanganui River Claims Settlement) Act 2017 No 7 (as at 12 April 2022)". www.legislation.govt.nz. Retrieved 3 September 2022.
  12. ^ Shuttleworth, Kate (30 August 2012). "Agreement entitles Whanganui River to legal identity". The New Zealand Herald. Retrieved 5 March 2023.
  13. ^ Fairbrother, Alison (18 September 2012). "New Zealand's Whanganui River Gains A Legal Voice". Huffington Post. Retrieved 5 March 2023.
  14. ^ Bauer, Winifred (2010). "The Wanganui/Whanganui Debate: A Linguist's View Of Correctness" (PDF). Victoria University of Wellington. pp. 8–9. Archived (PDF) from the original on 20 July 2020. Retrieved 21 July 2020.
  15. ^ Thomson, Arthur S. (1859). The Story of New Zealand, Past and Present, Savage and Civilised. Cambridge University Press. p. 37. ISBN 9781108039543. Retrieved 31 October 2020 – via Early New Zealand Books.
  16. ^ "Report for Altered District Name: Wanganui District to Whanganui District" (PDF). New Zealand Geographic Board. 29 April 2015. p. 6. Retrieved 13 June 2015.
  17. ^ "Whanganui or Wanganui – it's up to you". The New Zealand Herald. 18 December 2009. Retrieved 5 March 2023.
  18. ^ a b c "Whanganui National Park Management Plan 2012–2022" (PDF). Department of Conservation. Government of New Zealand. pp. 51–53. Retrieved 7 April 2023.
  19. ^ a b "Whanganui National Park: Nature and conservation". Department of Conservation. Government of New Zealand. Retrieved 7 April 2023.
  20. ^ Rainforth, Hannah Jane (2008). Tiakina Kia Ora – Protecting Our Freshwater Mussels (PDF) (Masters in Ecological Restoration). Victoria University of Wellington. Retrieved 14 November 2015.
  21. ^ Whanganui Catchment strategy (PDF). Palmerston North [N.Z.]: Horizons.mw. 2003. p. 5. ISBN 1-877310-29-8. Retrieved 14 November 2015.
  22. ^ Frost, P.G.H. "Nankeen night heron". New Zealand Birds Online. New Zealand Birds Online. Retrieved 14 November 2015.
  23. ^ DuFresne, Jim (2006). Tramping in New Zealand. Sixth ed. Lonely Planet. 392 pages. ISBN 1-74059-788-5, ISBN 978-1-74059-788-3
  24. ^ Hogan, C. Michael (2009). "Crown fern; Blechnum discolor". GlobalTwitcher.com.
  25. ^ "Hatrick, Alexander, 1857–1918". dnzb.govt.nz. Retrieved 5 March 2023.
  26. ^ "Paddle Steamer Waimarie, Whanganui". Retrieved 5 November 2017.
  27. ^ "Riverboat embarks on Whanganui voyage". One News. 18 June 2010. Retrieved 3 December 2011.
  28. ^ "adventurer.net.nz". Archived from the original on 13 January 2016.
  29. ^ Robin Hodge (2002). "The Scenic Reserves of the Whanganui River 1891 – 1986" (PDF). Waitangi Tribunal. Retrieved 5 March 2023.
  30. ^ a b "WANGANUI RIVER TRUST (ANNUAL REPORT OF THE); WITH MAPS". atojs.natlib.govt.nz. 1908. Retrieved 11 March 2022.
  31. ^ "BACK-COUNTRY SETTLEMENT. WANGANUI CHRONICLE". paperspast.natlib.govt.nz. 26 January 1918. Retrieved 11 March 2022.
  32. ^ a b c d e f "DEPARTMENT OF LANDS AND SURVEY (ANNUAL REPORT ON)". paperspast.natlib.govt.nz. 1898. Retrieved 10 March 2022.
  33. ^ "Te Araroa - Whakapapa - Manganui-o-te-Ao". www.teararoa.org.nz. Archived from the original on 30 June 2004.
  34. ^ Salisbury, Raymond (1997). East Cape to Cape Egmont – 80 day traverse of the North Island. Word for Word Publishing.
  35. ^ "Cycle bridge opens in time for summer". www.whanganui.govt.nz. Retrieved 19 December 2020.
  36. ^ "Whanganui mayor accepts blame for delays to Upokongaro Cycle Bridge". Stuff. 21 January 2020. Retrieved 19 December 2020.
  37. ^ "Upokongaro cycle bridge opening confirmed". www.whanganui.govt.nz. Retrieved 19 December 2020.
  38. ^ G. Gregg NZTA, P. Brabhaharan, J. Duxfield, S. Arumugam – Opus (April 2011). "Proceedings of the Ninth Pacific Conference on Earthquake Engineering – Retrofit to improve earthquake performance of bridge abutment slopes – COBHAM BRIDGE ABUTMENT RETROFIT USING DRILLED STONE COLUMNS" (PDF).{{cite web}}: CS1 maint: multiple names: authors list (link)
  39. ^ "Matapuna Bridge". www.heritage.org.nz. Retrieved 20 July 2020.
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