Wellington is the capital city of New Zealand. It is located at the south-western tip of the North Island, between Cook Strait and the Remutaka Range. Wellington is the third-largest city in New Zealand, and is the administrative centre of the Wellington Region. It is the world's southernmost capital of a sovereign state. Wellington features a temperate maritime climate, and is the world's windiest city by average wind speed.
Upper Hutt is a city in the Wellington Region of New Zealand and one of the four cities that constitute the Wellington metropolitan area.
The Hutt Valley campaign was an armed conflict in the lower North Island of New Zealand between indigenous Māori and British settlers and military forces in 1846. The campaign was among the earliest of the 19th century New Zealand Wars that were fought over issues of land and sovereignty. It was preceded by the Wairau affray and followed by the Wanganui campaign and was triggered by much the same pressures—the careless land purchasing practices of the New Zealand Company, armed government support for settler land claims, and complex intertribal tensions between local Māori. The three conflicts also shared many of the same combatants.
The 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.
The Wairarapa, a geographical region of New Zealand, lies in the south-eastern corner of the North Island, east of metropolitan Wellington and south-west of the Hawke's Bay Region. It is lightly populated, having several rural service towns, with Masterton being the largest. It is named after its largest lake, Lake Wairarapa.
Kaitoke, part of Upper Hutt City, is a locality in the southern North Island of New Zealand. It is located at the northern end of the Hutt Valley, 45 kilometres northeast of Wellington City and six kilometres from the northern end of the Upper Hutt urban area. It also lies at the southern end of the Tararua Ranges.
Petone, a large suburb of Lower Hutt, Wellington, stands at the southern end of the Hutt Valley, on the northern shore of Wellington Harbour. The Māori name Pito-one means "end of the sand beach".
Wellington Harbour is a large natural harbour on the southern tip of New Zealand's North Island. Central Wellington is located on parts of its western and southern sides, and the suburban area of Lower Hutt is located on parts of its northern and eastern sides.
Ngāti Toa, Ngāti Toarangatira or Ngāti Toa Rangatira, is a Māori iwi (tribe) based in the southern North Island and in the northern South Island of New Zealand. Its rohe extends from Whanganui in the north, Palmerston North in the east, and Kaikōura and Hokitika in the south. Ngāti Toa remains a small iwi with a population of only about 9000. It has four marae: Takapūwāhia and Hongoeka in Porirua City, and Whakatū and Wairau in the north of the South Island. Ngāti Toa's governing body has the name Te Rūnanga o Toa Rangatira.
Stokes Valley, a major suburb of the city of Lower Hutt in the North Island of New Zealand, lies at the edge of the city, seven kilometres northeast of the city centre. It occupies the valley of a small tributary of the Hutt River, called Stokes Valley Stream, which flows north to meet the main river close to the Taitā Gorge. Stokes Valley takes its name from Robert Stokes, who formed part of the original survey team of 1840 commissioned to plan the city at Thorndon in Wellington.
The Wairarapa Line is a secondary railway line in the south-east of the North Island of New Zealand. The line runs for 172 kilometres (107 mi), connects the capital city Wellington with the Palmerston North - Gisborne Line at Woodville, via Lower Hutt, Upper Hutt and Masterton.
The Hutt Valley Line is the electrified train service operated by Transdev Wellington on behalf of Metlink on the section of the Wairarapa Line railway between Wellington and Upper Hutt, New Zealand.
The Melling Branch is a railway branch line in the Hutt Valley, north of Wellington, New Zealand. It is part of the national rail network and formerly part of the Wairarapa Line. Until 2010 it was one of only two passenger-only lines in the country, since that year the two being joined by the Onehunga Branch and later by the Manukau Branch.
Te Āti Awa is a Māori iwi with traditional bases in the Taranaki and Wellington regions of New Zealand. Approximately 17,000 people registered their affiliation to Te Āti Awa in 2001, with around 10,000 in Taranaki, 2,000 in Wellington and around 5,000 of unspecified regional location.
Waterloo railway station is a dual-platform suburban railway station located in Lower Hutt, New Zealand, and serving immediately the suburbs of Waterloo, Lower Hutt Central and Woburn. The station stands on the Hutt Valley section of the Wairarapa Line, 15.5 km (9.6 mi) north of Wellington. Trains stopping at Waterloo run to Wellington, Taita, Upper Hutt and Masterton, as well as to points in between. Waterloo serves as a major bus-rail interchange, connecting buses to and from central Lower Hutt, Naenae and Wainuiomata with trains to and from Wellington.
Lower Hutt is a city in the Wellington Region of New Zealand. Administered by the Hutt City Council, it is one of the four cities that constitute the Wellington metropolitan area.
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.
Taranaki Whānui ki te Upoko o te Ika is a Māori collective that was formed to lodge claims with the Waitangi Tribunal relating to the New Zealand Company's purchase of land in the vicinity of Wellington in 1839 and 1844. Following on from the Tribunal's 2003 report WAI145, a settlement of these claims was signed in 2008 between the New Zealand Government and the collective.
Point Howard is a suburb on the eastern side of Wellington Harbour, in Lower Hutt, New Zealand.
The Waiwhetu artesian aquifer, sometimes referred to as the Hutt aquifer, is a pressurized zone of water-retaining sand, gravel and boulders beneath the Hutt Valley and Wellington Harbour in New Zealand. The aquifer provides about 40% of the public fresh water supply for Lower Hutt and Wellington city. Water from the Hutt River begins to flow underground south from Taita Gorge, then becomes pressurized under a seal of clay. Water is extracted from the pressurized area for public use, but concerns about overuse and damage by earthquakes have led to investigations of alternative sources of fresh water.
