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Big Muddy Creek (New Zealand)

Coordinates: 36°58′34″S 174°37′29″E / 36.9762°S 174.6247°E / -36.9762; 174.6247
From Wikipedia, the free encyclopedia

Big Muddy Creek
Big Muddy Creek seen from the Arataki Visitor Centre
Map
Route of the Big Muddy Creek
Big Muddy Creek (New Zealand) is located in Auckland
Big Muddy Creek (New Zealand)
Mouth of the Big Muddy Creek
Big Muddy Creek (New Zealand) is located in New Zealand
Big Muddy Creek (New Zealand)
Big Muddy Creek (New Zealand) (New Zealand)
Location
CountryNew Zealand
RegionAuckland Region
Physical characteristics
SourceLower Nihotupu Reservoir
 • coordinates36°57′44″S 174°36′57″E / 36.96209°S 174.61595°E / -36.96209; 174.61595
 • elevation65 m
MouthManukau Harbour
 • coordinates
36°58′34″S 174°37′29″E / 36.9762°S 174.6247°E / -36.9762; 174.6247
Basin features
ProgressionBig Muddy CreekManukau HarbourTasman Sea
Tributaries 
 • leftWilliams Stream, Finn Creek
 • rightShelly Lynn, Armour Stream

The Big Muddy Creek is an estuarine tidal inlet of the Auckland Region of New Zealand's North Island. It flows south from its tributary rivers, the Nihotupu Stream and the Island stream in the Waitākere Ranges which are dammed at the Lower Nihotupu Reservoir, towards the Manukau Harbour.

Geology

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Between 3 and 5 million years ago, tectonic forces between the Pacific Plate and Australian Plate uplifted the Waitākere Ranges and subsided the Manukau Harbour. Big Muddy Creek is likely a part of a fault-line that formed during this event. After the Last Glacial Maximum when sea levels rose, the river mouths of West Auckland flooded. While beaches formed at the mouths of Tasman Sea rivers, the relative lack of sand in the Manukau Harbour meant that Huia, Big Muddy Creek and Little Muddy Creek became tidal mudflats.[1]

History

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The creek was traditionally called Paruroa by Tāmaki Māori, meaning "wide mud", sharing meaning with the English language name.[2] The creek was important to Te Kawerau ā Maki, the mana whenua of the area, as a place where pātiki (flounder) could be netted.[3] Two Te Kawerau ā Maki kāinga (unfortified villages) existed in the area: Nihotupu, at Armour Bay close to the modern village of Parau, and Ngāmoko, near the Lower Nihotupu Dam.[3]

The creek was the site of the battle of Te-Rangi-hinganga-tahi, fought circa 1741 between the Te Taoū hapū of Ngāti Whātua, and Waiohua, then the major power on the Tāmaki isthmus.[4] After paramount chief Kiwi Tāmaki murdered guests at a funeral feast in Kaipara (modern-day Helensville), Te Taoū took revenge by attacking Waiohua-allied settlements on the Manukau Harbour.[4] The Te Taoū taua (war party) of 240 men, led by the chiefs Tuperiri, Wahaakiaki and Waitaheke, regrouped at Big Muddy Creek.[5][4] Kiwi Tāmaki, enraged at the attacks, formed a taua of thousands formed from across Tāmaki Makaurau, and descended on Big Muddy Creek.[6] Wahaakiaki ordered his warriors to adopt a feigned retreat, forcing the Waiohua force up the creek.[4] Despite being vastly outnumbered, Kiwi Tāmaki was defeated in battle and many of the demoralised Waiohua force died as they fled the battle.[4] The name of the battle, Te-Rangi-hinganga-tahi ("The Day When All Fell Together"), referred to the large number of corpses which polluted the Big Muddy Creek shellfish beds.[4]

Te Kawerau ā Maki remained in the area until 1825, when the Musket Wars forced most members of the iwi to flee to other regions in the country.[7] Many members of the tribe returned in 1836, first living at Huia to the west, before re-establishing a kāinga at Te Henga / Bethells Beach.[7] The land at Big Muddy Creek was sold to Europeans in the early colonial era of New Zealand without the knowledge of Te Kawerau ā Maki leaders.[7] From the 1830s until the 1920s, kauri trees were felled by European settlers for the logging industry in the southern Waitākere Ranges.[7] The coastal community of Parau developed on the western shores of Big Muddy Creek in the late 19th and early 20th centuries. In the latter half of the 19th century, the creek was occasionally referred to as Mangrove Creek.[8]

In the early 20th century, the creek was dammed with timber and later concrete structures.[7] The Lower Nihotupu Dam was constructed in 1948.[7]

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See also

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References

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  1. ^ Hayward, Bruce (2009). "Land, Sea and Sky". In Macdonald, Finlay; Kerr, Ruth (eds.). West: The History of Waitakere. Random House. pp. 13–14, 21. ISBN 9781869790080.
  2. ^ "Big Muddy Creek". New Zealand Gazetteer. Land Information New Zealand. Retrieved 30 April 2022.
  3. ^ a b Te Kawerau ā Maki; The Trustees of Te Kawerau Iwi Settlement Trust; The Crown (12 December 2013). "Deed of Settlement Schedule: Documents" (PDF). Retrieved 26 April 2022.
  4. ^ a b c d e f Stone, R. C. J. (2001). From Tamaki-makau-rau to Auckland. Auckland University Press. p. 36-45. ISBN 1869402596.
  5. ^ High Court of New Zealand (9 February 2021). "In the High Court of New Zealand: Auckland Registry CIV-2015-404-002033 Between Ngāti Whātua Ōrākei Trust and Attorney-General and Marutūāhu Rōpū Limited Partnership" (PDF). Retrieved 1 March 2022 – via Ngāti Whātua Ōrākei.
  6. ^ Campbell, Matthew; Furey, Louise (31 August 2011). "The NRD site I the archaeology report to the New Zealand Historic Places Trust and Auckland International Airport Ltd" (PDF). CFG Heritage. Retrieved 3 March 2022.
  7. ^ a b c d e f "The Muddy Creeks Plan – a Local Area Plan for Parau, Laingholm, Woodlands Park and Waimā" (PDF). Auckland Council. 13 February 2014. Retrieved 28 June 2021.
  8. ^ "Forty Acres of Heavy Bush - What Use Are They?". New Zealander. Vol. XVI, no. 1432. 7 January 1860. p. 3. Retrieved 27 April 2022 – via Papers Past.