Manukau Rovers RFC

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.

Māngere (Māori pronunciation: [ˈmaːŋɛɾɛ]) 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 City Centre and 15 kilometres south of the 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 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.

Auckland Seventh-day Adventist High School (ASDAH) is a secondary school (years 9–13) in Māngere Bridge, a suburb of South Auckland, New Zealand. It is owned by the Seventh-day Adventist Church. It is a part of the Seventh-day Adventist education system, the world's second largest Christian school system.

Centre Park is a stadium located in Mangere, Auckland, New Zealand. The stadium hosted the 2011 OFC U-20 Championship. It is the home of Northern League side Manukau United.

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. The area has a long history of habitation, due to its fertile lands, a productive harbour, and proximity to the Manukau-Tamaki isthmus. Māori of Ngāti Whātua were the inhabitants until they were supplanted by European farmers in the 19th century. The development of market gardening brought more people into the area and the land remained used in this way until the 1960s when housing developments were created to service Auckland's growing population and industry in nearby Onehunga and Otahuhu. Some areas of Favona also historically had large areas of greenhouses, such as for tomato production.The area is one is of relative poverty and until 2005 had one of New Zealand's largest Caravan parks. It hosts the Mangere campus of Te Wānanga o Aotearoa. Numerous shipping and freight forwarding companies have premises in the industrial areas, including the national distribution headquarters of supermarket chain Progressive Enterprises.

Māngere Lagoon is a lagoon in the Manukau Harbour, New Zealand. It occupies a volcanic crater or maar which is part of the Auckland volcanic field. Oval and about 600m long, it has a small restored scoria island remaining in the centre.

Hubbard Foods Ltd is a New Zealand manufacturer of breakfast cereals based in Auckland. It sells cereals under its Hubbard brand and private labels. Its founder is Dick Hubbard, who stepped down as CEO from 2004-2007 to serve as the mayor of Auckland. According to The Sunday Star-Times, in July 2010, Hubbard was "The number three player, behind Sanitarium and Kellogg's, in the so-called 'ready-to-eat' cereal market" in New Zealand. It employs around 150 staff.

Māngere Mountain 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 106 metres (348 ft) above sea level. It was the site of a major pā (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. It is also known as Te Pane-o-Mataaho ("the head of Mataaho"), and Te Ara Pueru ("the Path of Dogskin Cloaks").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. Many archaeological features remain, including kumara pits, garden terraces, walled garden mounds and stone boundary walls.Near the mountain to the southwest is Māngere Lagoon, filling another volcanic crater.

Waitomokia (also Moerangi, Gabriel Hill or Mount Gabriel) is a volcano in the Auckland volcanic field. Waitomokia's 600 m (2,000 ft) wide tuff crater contained three small scoria cones up to 20 m (66 ft) high, one with a crater, which were quarried in the 1950s.

Pukaki Lagoon, located in the suburb of Māngere, New Zealand, is one of the volcanoes in the Auckland volcanic field. The lagoon, alongside Māngere Lagoon, Waitomokia, Crater Hill, Kohuora and Robertson Hill, is one of the volcanic features collectively referred to as Nga Tapuwae a Mataoho ("The Sacred Footprints of Mataoho"), referring to the deity in Tāmaki Māori myths who was involved in their creation.Pukaki Lagoon has a 600 m wide explosion crater, with a surrounding tuff ring. After an eruption about 65,000 yrs ago the crater filled with freshwater and became a lake. It was breached by the sea as sea-levels rose after the end of the last ice age about 8,000 yrs ago and became a tidal lagoon. This was dammed and drained and used as a speedway from 1929 into the 1930s (Henning's Speedway). It is now farmland.

Southern Cross Campus (Te Kura Taki o Autahi) is a composite school that caters for students in Years 1-13 in the suburb of Mangere East in Auckland, New Zealand. The school (also referred to as 'SCC', 'The Campus' or 'The Cross') has deep ties to the Mangere East community by providing education, facilities, and programmes for the wider use of the whole school. It is a Māori and Pacific Islands ethnic school, with students of European (Pākehā), Asian, and other ethnicities as a 0.5% minority. Southern Cross Campus is a fairly new school to Auckland, by being an institute amalgamated with three previous schools in the area: Southern Cross Primary School, Mangere Intermediate School, and Nga Tapuwae College. Southern Cross Campus was founded by Terry Bates (MA (Hons), MPhil (Hons), DipTchg (NZ)), the first Campus Director of the school. It now comprises four schools: Southern Cross Junior School (Primary, Years 1–6), Southern Cross Middle School (Intermediate, Years 7–9), Southern Cross Senior School (Years 10–13), and Te Kura Māori o Ngā Tapuwae (a total-immersion school for Māori-language education, Years 1–13). In 2019, it was announced that after 13 years as Principal, Mr Robin Staples would retire at the end of Term 1 in the 2020 school year. He was succeeded at the beginning of Term 2 by Dr Samantha Smith, a former associate principal at Massey High School.

Boggust Park Crater is a volcano in the Auckland volcanic field, New Zealand. Located in the Favona area of the Māngere suburb, it is one of Auckland city's older volcanoes. It was first recognised as a volcano in 2011. The park in which it is located is named after Ralph Boggust, former superintendent of Manukau Parks Dept.The volcano has a 300–400 m diameter crater surrounded on three sides by a 6–8 m high semi-circular tuff ring with steep inner slopes and gentler outer slopes. In places the crest of the tuff ring has been flattened off by bulldozing during subdivision in the 1990s. The tuff ring is breached to the north-east, presumably by the sea during the Last Interglacial warm period, about 130,000 years ago, when the sea level was 5–6 m above the present. The present floor of the crater is about 5 m above present high tide level and slopes down to the edge of Harania Creek estuary on the Manukau Harbour. After eruption, Boggust Crater would have become a freshwater lake, before it was breached by the sea to become an intertidal lagoon for a few thousand years, rather like Panmure Basin today. The sea level dropped about 120,000 years ago and the crater became a swampy depression until 1 m of fill was added and drainage installed to make it a recreational sports field.