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  2. Wellington Fault - Wikipedia

    en.wikipedia.org/wiki/Wellington_Fault

    The Wellington Fault is an active seismic fault in the southern part of the North Island of New Zealand. It is a dextral (right-lateral) strike-slip fault with variable amounts of vertical movement causing uplift to the northwest, as expressed by a series of ranges.

  3. Pākuratahi River - Wikipedia

    en.wikipedia.org/wiki/Pākuratahi_River

    The Pākuratahi River, previously the Pakuratahi River, is a river of the Wellington Region of New Zealand's North Island. It flows northwest from its source in the Remutaka Range 15 kilometres (9 mi) east of Lower Hutt to join the Te Awa Kairangi / Hutt River near Kaitoke.

  4. Hutt River (New Zealand) - Wikipedia

    en.wikipedia.org/wiki/Hutt_River_(New_Zealand)

    The Hutt River (Māori: Te Awa Kairangi, Te Wai o Orutu or Heretaunga; officially Te Awa Kairangi / Hutt River) flows through the southern North Island of New Zealand. It flows south-west from the southern Tararua Range for 56 kilometres (35 mi), forming a number of fertile floodplains , including Kaitoke , central Upper Hutt and Lower Hutt .

  5. Hutt Valley - Wikipedia

    en.wikipedia.org/wiki/Hutt_Valley

    The Hutt Valley (or 'The Hutt') is the large area of fairly flat land in the Hutt River valley in the Wellington region of New Zealand. Like the river that flows through it, it takes its name from Sir William Hutt , a director of the New Zealand Company in early colonial New Zealand.

  6. Waiwhetu Aquifer - Wikipedia

    en.wikipedia.org/wiki/Waiwhetu_Aquifer

    The Waiwhetu aquifer covers a wedge-shaped area of 75 km² under the Hutt Valley and Wellington Harbour, and by size is the fifth-largest in New Zealand. [ 1 ] The harbour basin contains massive quantities of gravel washed down from the Hutt River, in some places hundreds of metres deep.

  7. Waiwhetū Stream - Wikipedia

    en.wikipedia.org/wiki/Waiwhetū_Stream

    The Waiwhetū Stream is a small watercourse in Lower Hutt, in the North Island of New Zealand. The stream drains the eastern side of the Hutt Valley, and enters Wellington Harbour at the Hutt River estuary. Development and urbanisation of the Hutt Valley since the arrival of settlers led to increasing pollution and degradation of the stream ...

  8. Tourist Who Narrowly Missed New Zealand Volcano Eruption ...

    www.aol.com/news/tourist-narrowly-missed-zealand...

    Man Who Missed New Zealand Volcano Eruption Shares Moments After

  9. Wainuiomata Water Collection Area - Wikipedia

    en.wikipedia.org/wiki/Wainuiomata_Water...

    Wainuiomata Water Collection Area is a reserve located near Wainuiomata, Lower Hutt in the Wellington Region at the southern end of New Zealand's North Island.It is administered by Wellington Regional Council, for exclusive use by Wellington Water as a water catchment reserve. [1]