Auckland Region Women's Corrections Facility

Matukutūreia (also McLaughlins Mountain) is one of the volcanic cones in the Auckland volcanic field. It has a peak 73 metres above sea level, and was the site of a pā. The scoria cone was originally crescent-shaped and featured Māori terraces and kumara pits, before extensive quarrying reduced it to a pyramid-shaped mound big enough to support the summit water tank for Papatoetoe. A small part of the summit and the eastern side of the cone were left unquarried, plus a large area of lava flows to the south of the cone remains intact. These remaining parts have recently been transferred to Department of Conservation Management, primarily because of the high heritage values of the Matukuturua Stonefields gardens. Matukutūreia and nearby Wiri Mountain are collectively known as Matukurua (also Ngā Matukurua).From July to September 2010, the water tank was removed from the top of Matukutūreia, as part of an agreement when the land was handed over to the Department of Conservation.

Matukutūruru (also Te Manurewa o Tamapahore or Wiri Mountain) is a volcano and Tūpuna Maunga (ancestral mountain) in Wiri, in the Auckland volcanic field. It had a scoria cone reaching 80 metres above sea level (around 50 m higher than the surrounding land), which was quarried away. The lava flows created 290m long Wiri Lava Cave. The hill was the site of a pā. In late 2011 the quarry lake was drained and fill-dumping began on the site.Matukutūruru and nearby Matukutūreia are collectively known as Matukurua (also ngā Matukurua).In the 2014 Treaty of Waitangi settlement between the Crown and the Ngā Mana Whenua o Tāmaki Makaurau collective of 13 Auckland iwi and hapu (also known as the Tāmaki Collective), ownership of the 14 Tūpuna Maunga of Tāmaki Makaurau / Auckland, was vested to the collective, including the volcano officially named Matukutūruru. The legislation specified that the land be held in trust "for the common benefit of Ngā Mana Whenua o Tāmaki Makaurau and the other people of Auckland". The Tūpuna Maunga o Tāmaki Makaurau Authority or Tūpuna Maunga Authority (TMA) is the co-governance organisation established to administer the 14 Tūpuna Maunga. Auckland Council manages the Tūpuna Maunga under the direction of the TMA.

Wiri lava cave is Auckland's longest known lava cave at around 290 metres. It is part of Matukutūruru (Wiri Mountain) volcano, in the Auckland volcanic field. Because it features rare lava stalactites the cave has garnered international renown. The cave entrance is locked and entry is by permit only. The cave is up to 7.6 by 3.6 m (25 by 12 ft), down to 1.1 by 0.2 m (3 ft 7.3 in by 7.9 in), and is located about 4 m (13 ft) below Wiri Station Rd.

Wiri railway station is a defunct station on the Southern Line of the Auckland Railway Network in New Zealand. To the north is Puhinui railway station and to the south is Homai railway station. Originally opened on 7 August 1913 as a "tablet station", and fully on 9 December 1913 as a siding and for staff and work trains (not a public station), the station closed on 14 February 2005 because it had the lowest patronage in Auckland.In July 2013, an extensive maintenance facility with stabling for 28 three-car trains was opened near the former station in preparation for the arrival of Auckland's new electric trains.The station is now used for train crew change in Wiri Depot Wiri is the start of the new Third Main Line to be completed by 2024.

The Puhinui Reserve is a protected working farm and wetland area in South Auckland, New Zealand, on the shores of the Manukau Harbour. It is the location of the Puhinui Craters, and is an area of historic significance to Waiohua iwi.

Ash Hill is a volcano in Wiri, in the Auckland volcanic field, in New Zealand. A low tuff cone with an explosion crater about 150m wide, it is now covered by industrial development. It peaked at roughly 30 metres above sea level (approximately 8 metres higher than the surrounding land). Ash Hill was named after nearby Ash Road by Searle. Ash Road was named after ash trees, not volcanic ash. Radiocarbon dating gave Ash Hill the age of 31,800 +/- 159 calendar years BP, a similar age to nearby Wiri Mountain.

The Puhinui Craters are located in Auckland's Puhinui Reserve and are part of the Auckland volcanic field in the North Island of New Zealand. They were first recognised as volcanic craters in 2011. A cluster of three small maar craters like these is unique in the Auckland volcanic field. Their ages are unknown but most probably all three erupted during the same eruptive episode. They could have been associated with the eruption of nearby Matukutureia (also known as McLaughlin's Mountain) but this is speculation at present. The cluster is composed of three maars, encircled by tuff cones that over tens of thousands of years have been partly breached and eroded by runoff from the small freshwater lakes appearing in the craters shortly after the eruption. Due to the maars' very gentle rise over the otherwise level terrace of Pleistocene age, their volcanic origin had not been recognised earlier. Puhinui Pond Crater, located near the reserve entrance, contains a farm pond. The crater is 200 m × 150 m (660 ft × 490 ft) across and the nearly complete surrounding tuff cone rim rises 1.5–2 m (4.9–6.6 ft) above the pond.Puhinui Arena Crater is breached on both the west and east sides. It is 250 m × 150 m (820 ft × 490 ft) across and its drained and sediment-filled flat floor is 2–2.5 m (6.6–8.2 ft) below the rim of the surrounding tuff ring.Puhinui Eroded Crater lies directly east of Arena Crater on the route of the small stream that drains the latter. Eroded Crater is breached at both west and east ends and its tuff cone partly eroded by the adjacent Puhinui Creek. It is less well-preserved than the other two craters but of similar size.

The Puhinui Creek, also known as the Puhinui Stream or Te Puhinui, is a major stream in South Auckland, in the Auckland Region of New Zealand's North Island. It flows westwards from Totara Park through Manukau, then southwest at Wiri to the Manukau Harbour.

Puhinui railway station is a station of the Auckland rail network and is located in Papatoetoe, Auckland, New Zealand. Passenger services on the Eastern Line and Southern Line use the station. It is accessed from Puhinui Road from both sides of the tracks via a pedestrian bridge located at the site of a former level crossing (Puhinui Road itself now crosses on a bridge approximately 120m north of the pedestrian bridge). This is the nearest public transport access to the main cemetery for South Auckland; Manukau cemetery at 361 Puhinui Road, Wiri. South of this station, Eastern Line and Southern Line services diverge, the Eastern onto the Manukau Branch which terminates at Manukau. The Southern continues south via Homai toward Papakura.

Clendon Park School is a primary school (Years 1–8) in Manurewa, a suburb of Manukau City, Auckland Region, New Zealand. Clendon Park has two bilingual units (Years 1–8). A Maori bilingual unit (Te Whanau Awhina) was established in 2000 and it currently consists of seven classes. The students in this unit often achieve above the national norms. A Samoan bilingual unit (Tautua Mo Tupulaga) began in 2006 and it currently comprises five classes.

Cemetery Crater is one of the volcanoes in the Auckland volcanic field. It is an explosion crater roughly 200 metres (660 ft) wide, located east of Crater Hill. Hard to see even in early aerial photos due to its shallowness, it is now covered by housing. It was first recognised by Ernie Searle in the 1960s. He named it because of its proximity to the cemetery in Puhinui Rd, but the Southwestern Motorway has now been constructed between the crater and the cemetery.

Baitul Muqueet Mosque is an Ahmadi Muslim mosque in Manurewa, Auckland, New Zealand. At the time of opening of the mosque, it was the largest mosque in the country.