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Māngere
Māngere () is a major suburb in South Auckland, New Zealand, located on mainly flat land on the northeastern shore of the Manukau Harbour, to the northwest of Manukau, Manukau City Centre and south of the Auckland CBD, Auckland city centre. It is the location of Auckland Airport, which lies close to the harbour's edge to the south of the suburb. The area has been inhabited by Tāmaki Māori since early periods of Māori history, including large-scale agricultural stonefields, such as Ihumātao, and Māngere Mountain, which was home to a fortified pā. Te Ākitai Waiohua communities in Māngere thrived in the 1840s and 1850s after the establishment of a English Wesleyan Mission, Wesleyan Mission and extensive wheat farms, until the Invasion of the Waikato in 1863. Māngere remained a rural community until the mid-20th Century, when Māngere became one of the largest state housing developments in Auckland. Etymology The name Māngere is a shortened form of the Māori languag ...
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Māngere Bridge (suburb)
Māngere Bridge is a suburb of Auckland, New Zealand, under the local governance of the Auckland Council. Surrounded by the Manukau Harbour, the area is the most north-western suburb of South Auckland, and is connected to Onehunga in central Auckland by Māngere Bridge (bridges), three bridges that cross the Māngere Inlet. Many features of the Auckland volcanic field are found in and around Māngere Bridge, including Māngere Mountain, a feature in the centre of the suburb, and Māngere Lagoon, a volcanic tidal lagoon opposite Puketutu Island in the harbour. The suburb is also home to Ambury Regional Park, a working farm and nature sanctuary run by Auckland Council, that connects to the Kiwi Esplanade and Watercare Coastal walkways. After being inhabited for hundreds of years by Tāmaki Māori, the area became a Ngāti Mahuta settlement to provide defense of Auckland from the late 1840s until the invasion of the Waikato in 1863. From later in the 19th century, Māngere Bri ...
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South Auckland
South Auckland ( or ) is one of the major geographical regions of Auckland, the largest city in New Zealand. The area is south of the Auckland isthmus, and on the eastern shores of the Manukau Harbour. The area has been populated by Tāmaki Māori since at least the 14th century, and has important archaeological sites, such as the Ōtuataua stonefield gardens at Ihumātao, and Māngere Mountain, a former pā site important to Waiohua tribes. The area was primarily farmland until the mid-20th century, when the construction of the Auckland Southern Motorway led to major suburban development, and the establishing of Manukau City, which was later amalgamated into Auckland. Large-scale State housing in New Zealand, state housing areas were constructed in the 1960s and 1970s, which led to significant Urban Māori and Pasifika New Zealanders, Pasifika communities developing in the area. The presence of 165 different ethnicities makes South Auckland one of the most diverse places in Ne ...
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Māngere East
Māngere East or Mangere East is a suburb of Auckland, New Zealand, under the governance of Auckland Council. It is located to the south of Favona, north of Papatoetoe, west of Middlemore, east of Māngere and Māngere Bridge, and southwest of Ōtāhuhu. In 2019, the name of the suburb was officially gazetted as Māngere East. Geography Māngere East is located in South Auckland, east of central Māngere between the Southwestern Motorway and the Southern Line. History The first evidence of Tāmaki Māori in the coastal Māngere area comes from the 14th century, with evidence of the first settlements later in the 15th century. The Māngere East area formed an important part of the Waokauri / Pūkaki portage, connecting the Manukau Harbour and Tāmaki River via Papatoetoe, and was often used by Tāmaki Māori to avoid the Te Tō Waka and Karetu portages, controlled by the people who lived at Ōtāhuhu / Mount Richmond. The area is within the rohe of the Waiohua tr ...
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Māngere Mountain
Māngere Mountain, also known by the names Te Pane-o-Mataaho and Te Ara Pueru, is a volcanic cone in Māngere, Auckland. Located within Māngere Domain, it is one of the largest volcanic cones in the Auckland volcanic field, with a peak above sea level. It was the site of a major pā (Māori people, Māori fortified settlement) and many of the pā's earthworks are still visible. It has extensive panoramic views of Auckland from its location in the southeastern portion of the city's urban area. Geography The volcano features two large craters. It has a wide crater with a lava dome near its centre, a feature shared by no other volcano in Auckland. It first erupted approximately 70,000 years ago. The mountain is one of the largest and best preserved of Auckland's volcanic cones. Most of the suburb of Māngere Bridge (suburb), Māngere Bridge was formed from the lava flows that came from the mountain's eruptions. Approximately 50,000 years ago, an eruption created hot fluid pāhoe ...
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Māngere-Ōtāhuhu Local Board
Māngere-Ōtāhuhu Local Board is one of the 21 local boards of the Auckland Council, and is overseen by the council's Manukau ward councillors. The board is governed by seven board members elected at-large. The board's administrative area includes the suburbs Māngere Bridge, Māngere, Ōtāhuhu, and Favona, and covers areas south of the Manukau Harbour. Geography The area includes the suburbs of Māngere and Ōtāhuhu, and the neighbouring suburbs of Māngere East, Favona and Māngere Bridge. Demographics Māngere-Ōtāhuhu Local Board Area covers and had an estimated population of as of with a population density of people per km2. Māngere-Ōtāhuhu had a population of 78,642 in the 2023 New Zealand census, an increase of 192 people (0.2%) since the 2018 census, and an increase of 7,683 people (10.8%) since the 2013 census. There were 39,096 males, 39,351 females and 198 people of other genders in 19,632 dwellings. 2.1% of people identified as LGBTIQ ...
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Favona
Favona is a mostly industry-dominated suburb of Auckland, New Zealand, and is part of the Māngere area. The suburb is in the Manukau ward, one of the thirteen administrative divisions of Auckland city, and is under governance of the Auckland Council. Etymology The origin of the name Favona is unknown, although it may relate to the cattle of the Robertson family who farmed in Māngere. Favona was the name of a race horse who came to prominence in the 1890s, who raised on John Lennard's farm in Māngere. In 1899 Hugh Mosman, member of the Queensland Legislative Council, purchased 300 acres of farmland in the area, calling his estate the Favona Farm. Geography Favona is located south of the Māngere Inlet, around the Tararata Creek and Harania Creek. The Boggust Park Crater in Favona is the oldest known feature of the Auckland volcanic field, erupting an estimated 130,000 years ago. History The first evidence of Tāmaki Māori in the coastal Māngere area comes from ...
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Auckland
Auckland ( ; ) is a large metropolitan city in the North Island of New Zealand. It has an urban population of about It is located in the greater Auckland Region, the area governed by Auckland Council, which includes outlying rural areas and the islands of the Hauraki Gulf, and which has a total population of as of It is the List of cities in New Zealand, most populous city of New Zealand and the List of cities in Oceania by population, fifth-largest city in Oceania. The city lies between the Hauraki Gulf to the east, the Hunua Ranges to the south-east, the Manukau Harbour to the south-west, and the Waitākere Ranges and smaller ranges to the west and north-west. The surrounding hills are covered in rainforest and the landscape is dotted with 53 volcanic centres that make up the Auckland Volcanic Field. The central part of the urban area occupies a narrow isthmus between the Manukau Harbour on the Tasman Sea and the Waitematā Harbour on the Pacific Ocean. Auckland is one of ...
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Auckland Airport
Auckland Airport is an international airport serving Auckland, the most populous city of New Zealand. It is the largest and busiest airport in the country, with over 18.7 million passengers served in the year ended December 2024. The airport is operated by Auckland International Airport Limited and is located near Māngere, a residential suburb, and Airport Oaks, a service-hub suburb south of the Auckland city centre. It serves as the principal hub for Air New Zealand, and the New Zealand operating base for Jetstar. The airport is one of New Zealand's most important infrastructure assets, providing several thousand jobs for the region. It handled 71 per cent of the country's international air passenger arrivals and departures in 2000. It is one of only two commercial airports in New Zealand that can handle Airbus A380 jet aircraft (the other being Christchurch). The airport has a single runway, 05R/23L, which is Cat IIIb capable (at a reduced rate of movements) in t ...
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Airport Oaks
Auckland Airport is an international airport serving Auckland, the most populous city of New Zealand. It is the largest and busiest airport in the country, with over 18.7 million passengers served in the year ended December 2024. The airport is operated by Auckland International Airport Limited and is located near Māngere, a residential suburb, and Airport Oaks, a service-hub suburb south of the Auckland city centre. It serves as the principal hub for Air New Zealand, and the New Zealand operating base for Jetstar. The airport is one of New Zealand's most important infrastructure assets, providing several thousand jobs for the region. It handled 71 per cent of the country's international air passenger arrivals and departures in 2000. It is one of only two commercial airports in New Zealand that can handle Airbus A380 jet aircraft (the other being Christchurch). The airport has a single runway, 05R/23L, which is Cat IIIb capable (at a reduced rate of movements) in the 23 ...
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Auckland Volcanic Field
The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island. The approximately 53 volcanoes in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With the exception of Rangitoto, no volcano has erupted more than once, but the other eruptions lasted for various periods ranging from a few weeks to several years. Rangitoto erupted several times and recently twice; in an eruption that occurred about 600 years ago, followed by a second eruption approximately 50 years later. The field is fuelled entirely by basaltic magma, unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taupō. Features The field ranges from Lake Pupuke and Rangitoto Island in the north to Matukutururu (Wiri Mountain) in the south, and from Mount Albert in the west to Pig ...
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Auckland Isthmus
The Auckland isthmus, also known as the Tāmaki isthmus, is a narrow stretch of land on the North Island of New Zealand in the Auckland Region, and the location of the central suburbs of the city of Auckland and the central business district. The isthmus is located between two rias (drowned river valleys): the Waitematā Harbour to the north, which opens to the Hauraki Gulf / Tīkapa Moana and Pacific Ocean, and the Manukau Harbour to the south, which opens to the Tasman Sea. The isthmus is the most southern section of the Northland Peninsula. The Auckland isthmus is bound on the eastern side by the Tāmaki River and by the Whau River on the west; two tidal estuaries of the Waitematā Harbour. These were used as portages by early Māori migration canoes and Tāmaki Māori to cross the isthmus (the Tāmaki River crossing known as Te Tō Waka, and the Whau River as Te Tōangawaka). Through early European settler history, canals were variously considered at either portage, h ...
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Manukau Harbour
The Manukau Harbour is the second largest natural harbour in New Zealand by area. It is located to the southwest of the Auckland isthmus, and opens out into the Tasman Sea. Geography The harbour mouth is between the northern head ("Burnett Head" / "Ohaka Head") located at the southern end of the Waitākere Ranges and South Head at the end of the Āwhitu Peninsula reaching up from close to the mouth of the Waikato River. The mouth is only 1800 metres wide, but after a nine kilometre channel it opens up into a roughly square basin 20 kilometres in width. The harbour has a water surface area of 394 square kilometres. There is a tidal variation of up to 4 metres, a very substantial change, especially since the harbour, being silted up with almost 10 million years of sedimentation, is rather shallow itself.Manukau Harbo ...
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