Pukekohe Hill | |
---|---|
Pukekohekohe | |
Highest point | |
Elevation | 222 m (728 ft) [1] |
Coordinates | 37°13′44″S174°53′36″E / 37.228917°S 174.893246°E |
Geography | |
Location | Auckland, North Island, New Zealand |
Geology | |
Volcanic field | South Auckland volcanic field |
Pukekohe Hill [2] (known traditionally as Pukekohekohe) [3] is one of the most prominent volcanoes of the South Auckland volcanic field in New Zealand. The shield volcano erupted approximately 550,000 years ago, making it one of the youngest known volcanoes of the field.
Pukekohe Hill is one of the youngest known volcanoes in the South Auckland volcanic field, erupting an estimated 550,000 years ago. [4] It is a gently-sloping shield volcano, which lies near the centre of the volcanic field. [5] The hill is composed almost entirely of basalt lava flows. [1]
The traditional Māori name Pukekohekohe ("Hill of Kohekohe") refers to Dysoxylum spectabile , also known as the New Zealand mahogany tree, which used to be a prominent part of the native bush on in the area. [3] Prior to European settlement, the hill was important to Waiohua tribes including Ngāti Tamaoho, Ngāti Te Ata and Te Ākitai, due to the strategic views and quality soil. The northern slopes of the hill were home to some of the largest croplands (māra kai) for the Tāmaki Māori people who settled here. [3]
In 1853, the hill became a part of Te Awa nui o Taikehu, a reserve the Crown created for Te Ākitai Waiohua during land sales. [3] After the Invasion of the Waikato, the land was confiscated in 1865, after which the European town of Pukekohe was built to the north of the hill. [3] The hill is the namesake of the town. [6] People who had lived in Te Awa nui o Taikehu returned to the area in the 1870s, often working as labourers in the market gardens on the former lands of the reserve. [3]
In the early 1900s, the northern slopes of Pukekohe Hill became the main source of potatoes and onion crops in New Zealand. The soil was renowned for being fertile, as three annual crops of potatoes and onions could be harvested annually. [5] The hill is one of the most prominent landforms in Pukekohe, and the peak was kept as a nature reserve, in order to preserve the scenic view at the peak. [1] The peak is topped with a grove of mature tōtara trees. [5]
Pukekohe is a town in the Auckland Region of the North Island of New Zealand. Located at the southern edge of the Auckland Region, between the southern shore of the Manukau Harbour and the mouth of the Waikato River. The hills of Pukekohe and nearby Bombay Hills form the natural southern limit of the Auckland region. Pukekohe is located within the political boundaries of the Auckland Council, following the abolition of the Franklin District Council on 1 November 2010.
Maungakiekie / One Tree Hill is a 182-metre (597 ft) volcanic peak and Tūpuna Maunga in Auckland, New Zealand. It is an important place culturally and archeologically for both Māori and Pākehā. The suburb around the base of the hill is also called One Tree Hill. It is surrounded by the suburbs of Royal Oak to the west, and clockwise, Epsom, Greenlane, Oranga, and Onehunga. The summit provides views across the Auckland area, and allows visitors to see both of Auckland's harbours.
South Auckland 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.
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 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.
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 106 metres (348 ft) above sea level. It was the site of a major pā 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.
Papakura is a suburb of South Auckland, in northern New Zealand. It is located on the shores of the Pahurehure Inlet, approximately 32 kilometres (20 mi) south of the Auckland City Centre. It is under the authority of the Auckland Council.
Taylors Hill, is a volcano in the Auckland volcanic field. It erupted about 33,000 years ago. Its scoria cone reaches 57 m (187 ft) high.
Robertson Hill is one of the volcanoes in the Auckland volcanic field in New Zealand. It erupted approximately 24,300 years ago. The hill, alongside Māngere Lagoon, Waitomokia, Crater Hill, Kohuora and Pukaki Lagoon, is one of the volcanic features collectively referred to as Nga Tapuwae a Mataoho, referring to the deity in Tāmaki Māori myths who was involved in their creation.
Ōwairaka / Mount Albert, also known as Te Ahi-kā-a-Rakataura, is a volcanic peak and Tūpuna Maunga which dominates the landscape of the Ōwairaka and Mount Albert suburbs of Auckland.
The Pukekiwiriki, also known as Red Hill, is the northernmost volcano of the South Auckland volcanic field in New Zealand, located east of Papakura, which erupted an estimated one million years ago. The hill was the site of a major Tāmaki Māori pā, and the Te Ākitai Waiohua village Te Aparangi in the 19th century.
Maungawhau / Mount Eden is a scoria cone and Tūpuna Maunga in the Mount Eden suburb of Auckland, New Zealand. The cone is part of the Auckland volcanic field, the tallest located on the isthmus.
Te Ākitai Waiohua is a Māori iwi of the southern part of the Auckland Region of New Zealand.
Te Waiohua or Te Wai-o-Hua is a Māori iwi (tribe) confederation that thrived in the early 17th century. The rohe was primarily the central Tāmaki Makaurau area and they had pā at Te Tātua a Riukiuta, Puketāpapa, Te Ahi-kā-a-Rakataura, Maungakiekie, Maungawhau, Tītīkōpuke, Ōhinerau, Rangitotoiti, Taurarua, Rarotonga, Ōtāhuhu, Te Pane o Mataaoho, Ihumātao, Matukutūreia and Matukutūruru, until the 1740s, when the paramount Waiohua chief, Kiwi Tāmaki, was defeated by the Ngāti Whātua hapū, Te Taoū. The descendants of the Waiohua confederation today include, Ngāti Te Ata Waiohua and Te Ākitai Waiohua.
Mataaho is a Māori deity. Variously considered a god of earthquakes and eruptions, the guardian of the earth's secrets, the god of volcanic forces, or a giant, Mataaho is associated with many of the volcanic features in the Tāmaki Makaurau Region. In traditional Tāmaki Māori myths, Mataaho either creates the volcanic features of the landscape, or requests the gods to create them. Mataaho holds traditional significance for Te Kawerau ā Maki and Waiohua iwi, and is considered a tupuna (ancestor) of Te Ākitai Waiohua and Ngaati Te Ata Waiohua iwi.
Āwhitu Regional Park is a regional park situated on the Āwhitu Peninsula, just south of Manukau Heads on the western side of the Manukau Harbour. It is situated in Franklin in Auckland in New Zealand's North Island, and is administered by Auckland Council.
Kiwi Tāmaki was a Māori warrior and paramount chief of the Waiohua confederation in Tāmaki Makaurau. The third generation paramount chief of Waiohua, Kiwi Tāmaki consolidated and extended Waiohua power over Tāmaki Makaurau, making it one of the most prosperous and populated areas of Aotearoa. Kiwi Tāmaki's seat of power was at Maungakiekie, which was the most elaborate pā complex in Aotearoa.
The Pūkaki Creek, also known as the Pūkaki Inlet, is an estuarine river of the Auckland Region of New Zealand's North Island. It flows south from its sources in Māngere and Papatoetoe, entering into the Manukau Harbour. The creek is adjacent to Auckland Airport and Pūkaki Marae.
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.
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.
The Pahurehure Inlet is an inlet of the Manukau Harbour of the Auckland Region of New Zealand's North Island. It is one of the three major inlets of the Manukau Harbour, alongside the Māngere Inlet and Waiuku Inlet.