Home  

Random  

Nearby  



Log in  



Settings  



Donate  



About Wikipedia  

Disclaimers  



Wikipedia





Canterbury Plains





Article  

Talk  



Language  

Watch  

Edit  





The Canterbury Plains (Māori: Kā Pākihi-whakatekateka-a-Waitaha[1]) are an area in New Zealand centred in the Mid Canterbury, to the south of the city of Christchurch in the Canterbury region. Their northern extremes are at the foot of the Hundalee Hills in the Hurunui District, and in the south they merge into the plains of North Otago beyond the Waitaki River. The smaller Amuri Plain forms a northern extension of the plains.

Aerial view of the Canterbury Plains
Location of the Canterbury Plains

Geology

edit

The Canterbury Plains were formed from Quaternary moraine gravels transported from the Southern Alps and deposited here during glacial periods in the late Pleistocene approximately 3 million to 10,000 years ago.[2] The alluvial gravels were then reworked as shingle fans of several of the larger rivers, notably the Waimakariri, the Rakaia, the Selwyn, and the Rangitata. Part of the Canterbury-Otago tussock grasslands, the land is suitable for moderately intensive livestock farming but is prone to droughts, especially when the prevailing wind is from the northwest. At these times, the weather phenomenon known as the Nor'west arch can be seen across much of the plain.

A major earthquake on 4 September 2010 revealed a previously unknown geological fault beneath the Canterbury Plains and created a surface rift that offset features by as much as four metres in places.[3]

Rivers

edit

The rivers of the Canterbury Plains have a distinctive braided appearance, which differentiates this area from the plains of North Otago to the south – beyond the Waitaki, the rivers typically have narrower, well-formed channels, rather than spreading across wide shingle depressions, as in Canterbury.

Most of the population of Canterbury lives in a series of large and small towns arranged northeast to southwest along the plains, connected by State Highway 1 and the Main South railway line. These include Christchurch, Ashburton and Timaru, and the smaller Kaiapoi, Dunsandel, Rakaia, Temuka, and Glenavy. Other towns on the plains include Rangiora, Leeston, Lincoln, Darfield, Geraldine, Methven and Waimate.

Fauna

edit

The extremely rare weevil Hadramphus tuberculatus is endemic to the plains.

References

edit
  1. ^ Taonga, New Zealand Ministry for Culture and Heritage Te Manatu. "The genealogy of the land". teara.govt.nz. Retrieved 18 July 2022.
  • ^ Gage, M., (1969), 'Rocks and Landscape', in The Natural History of Canterbury, edited by Knox, G. A., Canterbury Branch of the Royal Society of New Zealand, A H & A W Reed, Wellington, p. 35.
  • ^ Gorman, Paul (7 September 2010). "Fault awakens after 16,000 years of inactivity". The Press. Retrieved 27 January 2015.
  • 43°38′S 172°05′E / 43.64°S 172.09°E / -43.64; 172.09


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Canterbury_Plains&oldid=1218693902"
     



    Last edited on 13 April 2024, at 06:54  





    Languages

     


    Aragonés
    Cebuano
    Deutsch
    Español
    Français

    Norsk bokmål
    Norsk nynorsk
    Polski
    Português
    Русский
    Slovenščina
    Suomi
    Türkçe
    ئۇيغۇرچە / Uyghurche
     

    Wikipedia


    This page was last edited on 13 April 2024, at 06:54 (UTC).

    Content is available under CC BY-SA 4.0 unless otherwise noted.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Terms of Use

    Desktop