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Papatoetoe Panthers
Papatoetoe is a suburb in Auckland, New Zealand. It is the largest suburb in Auckland by population and is located to the northwest of Manukau Central, and southeast of Auckland CBD. Papatoetoe was traditionally an important area for Tāmaki Māori, who used a waka portage between the Tāmaki River and Waokauri Creek to reach the Manukau Harbour, as an alternative to the Ōtāhuhu portage to the north. The area developed as a farming community in the 19th century, and grew significantly in the 1950s and 1960s after the Auckland Southern Motorway was constructed. Papatoetoe is now known for its significant population of Indian New Zealanders. Etymology Papatoetoe means "grounds where toetoe grows", referring to species of ''Austroderia'' grasses that traditionally grew in the area. The name Papatoetoe was first used by English settlers from the 1850s onwards. The spelling Papatoitoi was common in English in the 19th century, and was gradually replaced with Papatoetoe after ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tāmaki River
The Tāmaki River or Tāmaki Estuary is mostly an estuarial arm and harbour of the Hauraki Gulf, within the city of Auckland in New Zealand.Eastern suburbs: Ōrākei to the Tamaki River (from Te Ara: The Encyclopedia of New Zealand. Accessed 2008-06-07.) It extends south for from its mouth between the suburb of Saint Heliers and the long thin peninsula of Bucklands Beach, which reaches its end at Musick Point. The inlet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mataoho
Mataaho (also known as Mataaoho and Mataoho) 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 (Auckland 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. Myths Myths of Mataaho are closely associated with many of the features of the Auckland volcanic field. The features were the creation of Mataaho and his brother Rūaumoko (the god of earthquakes and volcanoes), made as punishment against a tribe of patupaiarehe, supernatural beings living in the Waitākere Ranges, who used deadly magic from the earth to defeat a war p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crater Hill
Crater Hill is one of the volcanoes of the Auckland volcanic field, in New Zealand. It consists of an explosion crater about wide, partly filled with water. The hill, alongside Māngere Lagoon, Waitomokia, Kohuora Kohuora, located in the suburb of Papatoetoe, is one of the volcanoes in the Auckland volcanic field in the North Island of New Zealand. Geology and geography The Kohuora complex is a freshwater wetland found in a tuff ring, that has an explo ..., Pukaki Lagoon 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. Late in the eruption sequence lava welled up inside the explosion crater creating a lava lake. This lake began cooling on the surface and around the edge, creating a solid basalt crust. When the molten lava withdrew back down the volcano's throat, the crust surface collapsed, creating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kohuora
Kohuora, located in the suburb of Papatoetoe, is one of the volcanoes in the Auckland volcanic field in the North Island of New Zealand. Geology and geography The Kohuora complex is a freshwater wetland found in a tuff ring, that has an explosion crater around 600 metres wide and 30 metres deep. Kohuora erupted an estimated 34 million years ago, and the irregular V-shape of the complex indicated that there were at least three explosion crater vents. Peat and lacustrine deposits Lacustrine deposits are sedimentary rock formations which formed in the bottom of ancient lakes. A common characteristic of lacustrine deposits is that a river or stream channel has carried sediment into the basin. Lacustrine deposits form in all ... layer on top of the volcanic soil of the Kohuora. The Kohuora wetland is an important habitat for native bird and plant species, including '' Carex subdola'', a sedge rare in the Auckland area. History The volcano, alongside Māngere Lagoon, Waitomo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kohuora Explosion Crater 2009
Kohuora, located in the suburb of Papatoetoe, is one of the volcanoes in the Auckland volcanic field in the North Island of New Zealand. Geology and geography The Kohuora complex is a freshwater wetland found in a tuff ring, that has an explosion crater around 600 metres wide and 30 metres deep. Kohuora erupted an estimated 34 million years ago, and the irregular V-shape of the complex indicated that there were at least three explosion crater vents. Peat and lacustrine deposits Lacustrine deposits are sedimentary rock formations which formed in the bottom of ancient lakes. A common characteristic of lacustrine deposits is that a river or stream channel has carried sediment into the basin. Lacustrine deposits form in all ... layer on top of the volcanic soil of the Kohuora. The Kohuora wetland is an important habitat for native bird and plant species, including '' Carex subdola'', a sedge rare in the Auckland area. History The volcano, alongside Māngere Lagoon, Waitomo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austroderia
''Austroderia'' is a genus of five species of tall grasses native to New Zealand, commonly known as toetoe (from Māori).Toetoe hosted on the NZ Landcare research Maanaki Whenua website. Page accessed 20 November 2010. The species are ''A. toetoe'', ''A. fulvida'', ''A. splendens'', ''A. richardii'' and ''A. turbaria''. They were recently reclassified in 2011 from the genus '''', although their distinctiveness had been recognized as early as 1853. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
